T H E U N I V E R S I T Y OF M I C H I G A N COLLEGE OF ENGINEERING Department of Meteorology and Oceanography Technical Report OBSERVED LAND AND LAKE BREEZE CIRCULATION ON THE EASTERN SHORE OF LAKE MICHIGAN, 25 JUNE, 1965 Lars E. Olsson, Alan L. Cole, and E. Wendell Hewson Aksel Wiin-Nielsen, Project Director ORA Project 08650 Supported by: DEPARTMENT OF HEALTH, EDUCATION, AND WELFARE PUBLIC HEALTH SERVICE DIVISION OF AIR POLLUTION GRANT NO. AP 00380-01,02,03 WASHINGTON, D. C. administered through: OFFICE OF RESEARCH ADMINISTRATION ANN ARBOR October 1968

A C KNOWL E DG EM E NT S The authors wish to express their sincere appreciation of the work of several persons in the execution of this study. In particular Prof. G C. Gill for his assistance in selection of instruments and Messrs. F 'Brock and A. Stohrer for their work in the field and in the data processing. The tower and instrument shelter location at the shore of Lake Michigan provided by the Water Department of the City of Grand Rapids, Michigan constituted an ideal lakeshore observation site. The generosity of this department is gratefully acknowledged. Thanks is also given to Mr. D Haig, the captain of the R/V MYSIS for his excellent assistance in the observational program on Lake Michigan. The writers also gratefully acknowledge the work done by Mrs. Anna L. DeRey, Mrs. Karen Tingle and Mr. Dirk Herkhof in abstracting and preparing the data. Thanks is also given to Mrs. Bonnie Nuttall and Mrs. Ruthie Tolbert for typing the many tables and the original manuscript and to Dr. Valentin Vitols for reading the manuscript and making useful suggestions. ii

TABLE OF CONTENTS Page LIST OF TABLES o 0 0 0 0 O e iv LIST OF FIGURES...O *.. O.. *.. *.. *. v ABSTRACT ix ABSTRACT e eb e e b T b o e ~ dp O f ** e e * * o *, * iX 1. INTRODUCTION..................... 1 2. LOCATION OF STUDY AND OBSERVATIONAL PROGRAM.,. e 0o o o.. o.o 0...**... * o. ** 4 3 PREVAILING METEOROLOGICAL CONDITIONS 25 June,;1965 *00.......0.... 21 4. OBSERVED TEMPERATURES, HUMIDITIES, AND WINDS...................... * 33 4.1 Temperature and Moisture.... 33 402 The Lake and Land Breeze Circulation................ 44 4.3 Summary. o.............. 65 5. A COMPREHENSIVE SUMMARY OF PREVIOUSLY REPORTED OBSERVATIONAL STUDIES OF LAND, LAKE, AND SEA BREEZE CIRCULATIONS...~........... 71 6. CONCLUSIONS 80 REFERENCES........................ 81 APPENDIX..oO. O..o. 85 iii

LIST OF TABLES Table Page A summary of available winds aloft observations for 25 June, 1965.................... 19 2 Local times for lake breeze frontal passage at various stations as detected in wind direction change, temperature drop, and dew point rise near the surface on 25 June, 1965. o.... o Al Dry bulb temperature, relative humidity, dew point temperature, and solar radiation for several stations near an observation line south of Grand Haven, Michigan on 25 June, 1965. o o.. 86 A2 Air and soil temperature at various heights respective depths at the WJBL station north of Holland Michigan, 25 June, 1965.......... a 87 A3 Dry and wet bulb temperatures, relative humidity, and water vapor pressure observed from aircraft on 25 June, 1965 south of Grand Haven, Michigan.. 88 A4 Wind directions and wind speeds for several stations near an observation line south of Grand Haven, Michigan on 25 June, 1965. 92 A5 Analyses of pibal observations made at stations along an observation line south of Grand Haven, Michigan on 25 June, 1965 t eoe b o o *eK iv 93 iv

LIST OF FIGURES Figure Page 1 Location of observation stations on the eastern shore of Lake Michigan.,....*......**.**.. 5 2 Lake shore stationo......*... 7 3 Lake shore theodolite site...... 7 4 Meteorological tower at 8 km station *....................~* 9 5 Esterline-Angus 20 pen event recorder for wind speed and direction recording and Messenger II, 5 watt Citizen's Band radio telephone e................*... 9 6 Theodolite site at 8 km station. 11 7 WJBL TV tower................... 11 8 Fritiz aerometeorograph, mounted on left wing strout of Cessna 172 aircraft.................... 13 9 Yellow Spring Instrument Corporation Thermistors, mounted on right wing strout of Cessna 172 aircraft.~ o..................,... 13 10 ER/V MYSIS e *.........e........14 11 U.S. Weather Bureau Daily Weather Map for 25 June, 1965.......... 22 12 Mesoscale surface weather map and station weather at 0700 EST, 25 June, 1965.................. 23

LIST OF FIGURES (continued) Figure Page 13 Mesoscale surface weather map and station weather at 1300 EST, 25 June, 1965............. 24 14 Mesoscale surface weather map and station weather at 1900 EST, 25 June, 1965.................. 25 15 Height contours for the 850 mb surface at 1900 EST, 24 June,i 1965.. o o o. o o 26 16 Height contours for the 850 mb surface at 0700 EST, 25 June, 1965 o........................... 27 17 Height contours for the 850 mb surface at 1900 EST, 25 June, 1965.. o o o o 28 18 Height contours for the 700 mb surface at.1900 EST, 24 June, 1965 o o e... o o o o a o o o 29 19 Height contours for the 700 mb surface at 0700 EST, 25 June, 196500 0.... o 9 0 0................. a 30 20 Height contours for the 700 rrb surface at 1900 EST, 25 June, 1965 o o o o o. e o....... 31 21 Solar radiation recorded at the Lake shore station on 25 June, 1965.0........................ 32 22 Lapse rates and soil temperature as a function of time at WJBL tower on 25 June, 1965 oo........o 34 vi

LIST OF FIGURES (continued) Figure Page 23 Lapse rates over lake and over land at various times on 25 June, 1965. Aircraft soundings *...... 35 24 Analyzed vertical temperature field in early morning, 0737 -0908 EST, 25 June, 1965......... 37 25 Analyzed vertical temperature field in late morning, 0953 -1121 EST, 25 June, 1965......... 38 26 Analyzed vertical temperature field in early afternoon, 1232 -1404 EST, 25 June, 1965........ 39 27 Temperature as a function of time at various stations on 25 June, 1965..... ee............. 40 28 Dew Point temperature as a function of time at various stations on 25 June, 1965....... 43 29 Isotachs for the across-shore component (U) at 0830 EST, 25 June, 1965.......... 0. oes.. 45 30 Isotachs for the along-shore component (V) at 0830 EST, 25 June, 1965................... 46 31 Isotachs for the across-shore component (U) at 1100 EST, 25 June, 1965....... 47 32 Isotachs for the along-shore component (V) at 1100 EST, 25 June, 1965.. o.......... 48 vii

LIST OF FIGURES (continued) Figure Page 33 Isotachs for across-shore component (U) at 14 00 EST, 25 June, 1965.....o.......... o 49 34 Isotachs for the along-shore component (V) at 1400 EST, 25 June, 1965..0.0..0.0.0...... 50 35 Isotachs for the across-shore component (U) at 1700 EST, 25 June, 1965.o................ 51 36 Isotachs for the along-shore component (V) at 1700 EST, 25 June, 1965.................. 52 37 Isotachs for the across-shore component (U) at 1900.FST, 25 June, 1965........ o o. o.. 53 38 Isotachs for the along-shore component (V) at 1900 EST, 25 June, 1965.... o o.......... 54 39 Across shore wind component (U) as a function of height at various times and stations, 25 June, 1965................. 55 40 Wind vectors at the surface, 200 mand 1050 m aloft at various times an~d at various stations 25 June, 1965........ 56 viii

ABSTRACT An observational study carried out near Grand Haven, Michigan on 25 June, 1965 has produced probably the most extensive measurements available of a nearly idealized land and lake breeze circulation. The complete cycle of nocturnal land breeze to lake breeze during the day with a return to land breeze at night was observed and measured. These data constitute field measurements that are available for the guidance of theoretical studies and for the experimental evaluation of proposed lake breeze models. The synoptic situation is documented and several mesoscale analyses presented. Several graphs describing winds and temperatures as functions of time and space are included as is a graph indicating moisture change at various stationso The penetration of the lake breeze front is measured by wind, temperatures and moisture changes Temperature lapse rates, wind profiles, and their variations are presented. A comprehensive summary of previously reported observational studies of land, lake, and sea breeze circulations is reported.

1 ~ INTRODUCTION The effects of mesoscale meteorological phenomenon on large scale circulation, local climate, air pollution dispersion, etc., have received increased attention in recent years. The air-sea interactions and the effects of the land-water transition on energy transfers in the atmospheric boundary layer and on mesoscale circulations are just beginning to be understood. Since 1963 the Department of Meteorology and Oceanography at the University of Michigan has been conducting observational studies of the mesoscale wind circulation and related temperature and moisture structure near the southern basin of Lake Michigano Intensified studies have been conducted mainly during spring and early summer, when the daytime temperature difference between land and water is at a maximum and well defined lake breeze circulations occur. One particularly well documented lake breeze, which occurred on the eastern shore of Lake Michigan on 25 June, 1965, is presented in this report. A summary of these observations has been presented by Olsson, Cole and Hewson (1968). Munn and Richards (1964) have used climatological records to show lake breeze -1 -

-2 -occurrences at a location near Lake Huron. They have also described typical lake breeze circulation features. Moroz (1965, 1967), using observational methods similar to those presented in this report, has described a lake breeze on the eastern shore of Lake Michigan. The main difference between his description and the one presented here is the resolution of data in time and space. While Moroz had to synthesize "'a lake breeze day"' from observations taken on days with similar synoptic situations this report documents one day with the nocturnal land breeze reversed to a daytime lake breeze and the return to a land breeze in the eveningo Strong (1968) and Strong and Bellaire (1967). have observed and discussed lake effects and lake breezes over and near Lake Michigano Hewson and Olsson (1967) have summarized various lake effects and their influence on air pollution dispersion. Estoque (1961) has produced a two dimensional numerical model for the sea breeze into which he later imposed a gradient wind (1962) and McPherson (1968) has expanded this model into three dimensions. Moroz (1965) has developed a two dimensional numerical model for the lake breeze under zero gradient wind conditions. Strong (1968) has

-3 -shown that with a gradient wind of more than 5 m sec 1 a Great Lake is of sufficient size to be modeled as an ocean and Estoque's numerical model becomes "valid" also for the lake. Upper air soundings and surface weather information from stations surrounding the Great Lakes indicate that the gradient winds for 25 June, 1965 were in general less -1 than 5 m sec o While several authors have contributed to the knowledge and understanding of sea, lake, and land breezes, only a few have undertaken to observe the development of those circulations in space and time. Besides the observations of lake breezes mentioned above, Fisher (1960), Frizzola and Fisher (1963), and Angell and Pack (1965) have reported on recent sea breeze observations at middle latitudes. Sea breezes in the tropics have been observed and described by van Bemmelen (1922), and Dixit and Nicholson (1964). Wexler (1946) and Defant (195l1)have summarized the main features of land and sea breezes and Fujita (1965) has published a bibliography including most lake and sea breeze studies. A summary of the findings made in these earlier observational studies will be made later in this report.

2. LOCATION OF STUDY AND OBSERVATIONAL PROGRAM Observations were made at a site on the eastern shore of Lake Michigan near Grand Haven, Michigano The relative location of the site and the observational stations of primary concern are indicated in Figure 1. The coordinate system used throughout this report is such that the x-axis coincides with "~the observation line " along Michigan highway 45 (M-45) and is positive to the east, the y-axis coincides with the coast south of origin (the intersection of M-45 and shore line) and is positive to the north. The altitude of the ground surface is everywhere set to be zero and the z-axis is positive upward. The site selected offers several distinct advantageso The lake is long and narrow (approximately 110 km wide) with its axis running nearly north-south, the curvature of the shoreline is small and does not strongly modify the flow patterns and along shore homogenity can for all practical purposes be assumed in the neighborhood of the observation line. Sand dunes run parallel to the sand beach, with heights of up to 50 meters above mean lake levelO The dunes are in general confined to within 1 km from the shore, and =4 -

J 1 MUSKEGON LLAK ~~MKG LAKE TOWER I___________ _ U..._ MILWAUKEE GRAEN GRANDHV HAVEN CHICAGO o wJBL FIGURE 1. Location of observation stations on the eastern shore of Lake Michigan. Insert shows the location of the line of observations relative to Lake Michigan. Insert show1s the location of +%-he line of observations relative to Lake Michigan

-6 -are partly covered with trees. Two or three km inland from the lake the land becomes flat and is uniformly developed for agriculture. The slope of the land from Grand Rapids toward the lake shore is small (approximately. 1/1000) and it is assumed that no slope winds develop. A short description -of the stations and their instrumentation follows: Lake shore station (0 km) was located on the lawn at the Grand Rapids pumping station, in a 200 m wide break in the sand dune chain. A USWB-type instrument shelter was located on a lawn 50 m from shore, 15 m above mean lake water levell and 20 m lakeward (west) of the 10 m high pumping station0 Figure 2. Temperature and relative humidity were recorded on a Bendix Friez Model 594 recording hygrothermograph in the shelterO Due to a failure in the recording device, no surface winds were obtained for 25 June. The winds used as representative for this station are averaged from observations obtained from nearby U.S. Coast guard stations. Winds aloft were measured by either single or double theodolite tracking of pilot balloonso Figure 3 shows a theodolite crew at work at the lake shore station. The theodolites

FIUR 2. Lake shore staion An lJSWItyp in FIGURE 3. The north t heodolite site at the Lake shore station viewed from the south-east. Lake Michigan in the background.

-8 -were located on the beach, south of the station, with a 305 m (1000 ft) north south baseline. A Belfort Recording Pyrheliometer was located on the roof of the pumping station, approximately 10 m above the ground. 8 km station was located on a farm in flat terrain. A USWB-type instrument shelter, located approximately 100 m east of the farm buildings, housed a Bendix Friez Model 594 hygrothermograph. Close by the shelter, on the 12.2 m level of a 24.4 m guyed steel tower was located a Science Associates #418 wind direction sensor and a Science Associates #402 anemometer, Figure 4. Wind speed and direction were recorded on an Ester lineAngus 20 pen event recorder, Figure 5. Two theodolites were located on an open field to the south of the station with a 305 m northsouth baseline, Figure 6. 16 km station was located on the lawn of a field station of the Michigan Department of Conservation. The lawn was shielded from open fields by hedges to the north and west, and by a small built-up area to the southeast. A USWB-type instrument shelter with a Bendix Friez Model 594 recording hygrothermograph and a 12.2 m guyed steel tower with a top mounted Science Associates #418 wind direction

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-10 -sensor and Science Associates #402 3-cup anemometer was located on the lawn. Wind speed and direction were recorded on an Esterline-Angus 20 pen event recorder. A station for single theodolite tracking of pibals was located on an open field south of the conservation station. 24 km stationr, with a Bendix Friez Model 594 recording hygrothermograph in an USWBt type instrument shelter, was located with open fields towards south and with wooded areas toward north. WJBL station is a radio station located north of Holland, Michigan; x = 10 km and y = -17 km. The sensors were mounted on a 91.4 m high radio transmitting tower located on an open field, Figure 7. Copper constantan thermojunctions; in Thornthwaite shields at the 2.4, 4.9, 9.8, 19.5, 39.0, and 78.0 m levels sensed air temperatures and copper constantan thermojunctions at 0.01, 0.10, and 1.00 m depths in the ground sensed soil temperatures. These temperatures were recorded on a Honeywell-Brown multipoint recorder. Electric Speed Indicator 3-cup anemometers and wind vanes type F-420-C were mounted at the 19.5, 39.0, and 78.0 m levels. Wind speeds and directions were

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-12 -recorded on Esterline-Angus 0-1 ma dual stripchart recorders. Airplanes, type Cessna 172, flew trajectories in a vertical plane along the observation line. They were equipped with Friez aerometeorographs for temperature and relative humidity recording, Figure 8, and with Yellow Spring Instruments Corporation thermistors, mounted in radiation shields, for instantaneous readings of air temperature and wet bulb temperature, Figure 9. MYSIS is a fifty foot, steel hulled research vessel belonging to the Great Lakes Research Division of the Institute of Science and Technology, University of Michigan, Figure 10. She operated mainly 1.6 to 6.4 km off shore along the observation lineo Bow and beam winds with respect to the vessel were measured with an Electric Speed Indicator 3-cup anemometer and wind vane type F-240-C mounted on the top of the shipis mast, 12.1 m above water surface. Air temperature was measured with a Rosemont Engineering platinum resistance thermometer system with sensors mounted in Thornthwaite-type radiation shields 11.8 m above water on the mast and at 5.1 m above water on the bowsprit. Water temperature was sensed at 1.2 m under the water surface. Humidity was

FIGURE 8. A Fritz aerometeorograph, mounted on left wing strout of a Cessna 172 aircraft. a 1esn 172 ai1at S 1}}111 * ~~~~~~~~~~~~~~~~~~~~~~~~~~~BBI?/! i ii8 x... AiB}ia W ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~i:iiS4:ii!' '-"''" ~ 0'''S ' FIGURE 9. Yellow Spring instr~ument Corporation TPhermistorst for dry and wetbulb temperaturce sensi~ng, in radliatio3n shield mounted on:rightt wing strout of a Cessna 172 aircraft.

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-15 -sensed with a Honeywell lithium chloride dew probe on a bow mounting at 5.0 m above the water. Solar radiation was sensed by an Eppley solar radiation sensor mounted on top of the wheelhouse. Ship speed and heading were set manually, as was the date, while a digital clock produced time signals with one minute resolution. All instruments onboard the MYSIS were recorded on an Information Instruments Inc. data logger model 641. This data logger converts analog voltage signals to digital form and records them on punched paper tape. Sampling time was in the order of milliseconds, with each sensor sampled and recorded once per minute. Releases of pilot balloons, for either shipboard tracking with marine theodolite or shoreline tracking. with standard theodolites, were made. All instruments on the previously mentioned stations were checked frequently and corrected, e.ogo the hygrothermographs were checked once a day against sling psychrometers. Communication between the different observational sitess was provided by three Messenger II, and one Hallicrafters transistorised, 5 watt, Citizen's Band radio telephones. At the locations for double theodolite tracking, field tele

-16 -phones and buzzers were used between the two theodolites for coordination and timing. Smoke plume generation and smoke plume photography as well as measurements of wind fluctuation with Gill anemometer bivanes were made at various observational sites. Results of these findings will be reported elsewhere. MKG is a USWB station located on the eastern side of Muskegon airport, 6.5 km inland from the shoreline, at coordinates x = 0, and y = 21 km. GRR is a USWB station located at Grand Rapids airport at x = 53 and y = -10 km. Both MKG and GRR make routine observations on the hour. Lake Tower is a research tower belonging to the Great Lakes Research Division and located at x = -7 and y = 22 km, 1.8 km off shore, Elder (1964). Windspeeds and directions are sensed by an Aerovane mounted 15 0 m above water and recorded on a data logger. Auxiliary observations made at USWBstations, U.S. Coast Guard stations, and onboard ships on the Great Lakes have been used in describing the synoptic situation and in evaluating the large scale situation, but are not tabulated in this report.

-17 -Most of the data presented in this report have been abstracted and analyzed at the Department of Meteorology and Oceanography of the University of Michigan, and are punched on IBM cards. Some of the data are stored on magnetic tape. Temperature, humidity, wind, and radiation data are tabulated and presented as appendices in this report. At WJBL a temperature is recorded on a twelve point recorder at one half minute intervals, thus making a recording of the temperature at each level every six minutes. The temperature record was abstracted by reading one cycle of recordings at half hour intervals. Temperatures and relative humidities at the Lake shore, 8 km, 16 km, and 24 km, stations were read from hygrothermograph-charts as "preceding 1/2 hour averages"' or "preceding 1 hour average~". Dew point temperatures at these stations were obtained from tables. Winds at the WJBL, 8 km, and 16 km stations are read from strip charts as "'preceding 1/2 hour averages go or preceding 1 hour averages"" Winds at the lake shore were estimated averages from neighboring U.S. Coast Guard. stations, while solar radiation for the station was taken from the pyrheliometer

-18 -chart as 00centered 1/2 hour averages " Wind data from the Lake tower were taken as "'centered 1 hour averages ". Data from MYSIS were taken as "centered 5 minutes averages., on every half hour, from the print out of the datalogger's punched papertape, whenever the ships location so warranted. Data from MKG and GRR were taken from these USWB stations hourly observation records. Dry bulb and wet bulb temperatures obtained from the airplane flights were read from the Yellow Spring Instrument recorder as instantaneous values at height increments of 152 m.Corresponding times and horizontal distances (xvalues) were given. Relative humidity was obtained from psychrometric tables and vapor pressure was computed. Winds aloft data were determined from theodolite tracking of pilot balloons. Analyses of the tracks were made on a digital computer. The analysed runs are summarized in Table 1, and components across shore (u), along shore (v), total horizontal (VT), and in the cases of double theodolite tracking, vertical winds (w) are listed in Table A5 together with balloon coordinates (x,y,z) at any given time after balloon release.

-19 -TABLE 1. A summary of available winds aloft observations for June 25, 1965. "'D" indicates that double theodolite tracking and analyses were used and "IS" that single theodolite analyses were made. Superscript 1 indicates 0"balloon released from MYSIS", from distance off shore as given in km in MYSIS column. Numbers in brackets are duration of track in minutes. Time Lakeshore 8 KM 16 KM MYSIS 0600 D (20.0) 0630 S (13 0) S (20.0) -1.6*) 0700 S (20.0) 0700 S (20.0) *) Not tracked 0730 S (20.0) from MYSIS 0800 D (20.0) S (20.0) 0830 D (20.0) S (20.0) 0900 S1(20.0) S (20.0) -1.6 (12.5) 0930 D (20.0) S (20.0) 1000 D (20.0) S (20.0) 1030 D (20.0) S (20.0) 1100 D (13.0) D (20.0) -6.4 (1205) 1130 D (19.5) D (20.0) 1200 D (20.0) D (20.0) -1.3 (12.5) 1230 S (20o0) S (20.0) 1300 S (20.0) S (20.0) 1330 D (20.0) D (20.0) 1347 -6.4 (12.5) 1400 D (20.0) D (1800) 1430 D (20.0) D (17.0) 1500 S (20.0) D (20.0) 1530 S (20.0) D (15.0) 1600 S (20.0) D ( 6.0) S (20oO) 1630 S (2000) D (15.0) 1700 S (20~0) D (15.0) S (15.0) 1730 S (2000) S (15.0) 1800 D ( 9o0) D (15.0) S ( 7.0) S (20,0) 1830 D (20~0) D (11.0) S ( 8.5) 1900 D (20.0) D (15.0) S (14.5) 1930 S (15.0) 1945 D (20o0) 2000 S (15.0) 2015 s ( 8.5) 2030 D (6o5) s (1So5)

30 gram balloons, inflated at land stations with hydrogren to have an ascent rate of 183 m min (600 ft min ) and onboard the ship with helium (for safety reasons) to have an ascent rate of 180 m min, were used. Theodolite observations were made at 1/2 minute intervals to permit analysis for winds through thin layers in order that details of flow changes with height could be discerned. No weighting functions were used to smooth the data, although some smoothing is introduced by using the conventional technique of averaging over two layers to evaluate the wind at the midpoint. As can be seen from Table 1 some of the balloon flights were analysed, both as double and as single theodolite runs in order to determine errors made by assuming a constant ascent rate. These comparisons showed that the inherent error of wind analyses using single theodolite observations in very few cases exceeded + 1 m sec for land based theodolites and only in cases of balloon elevations over 1500 meters for the shipboard theodolite. In general the accuracy estimated by Frizzola and Fisher (1963) and -1 by Moroz (1965) of + 2 m sec for single theodolite observations in sea and lake breezes, respectively, holds for the results presented here.

3 PREVAILING METEOROLOGICAL CONDITIONS, 25 JUNE, 1965. On 25 June, 1965 the Lake Michigan basin was under the influence of a cold surface high, with a very weak pressure gradient over the entire Great Lakes region, Figure 11. During the day "mesoscale lake highs" developed over Lake Michigan and Lake Huron. In the late afternoon these highs had reached intensities of 3 - 4 millibars, Figures 12 - 14. Surface winds around Lake Michigan were light and variable in the morning hours. In the afternoon the surface winds reported from stations close to the shore, i.e. Muskegon, Chicago, Milwaukee, and Escanaba indicate lake effects around the entire lake. Similarly surface winds from stations around the other Great Lakes show clear evidence of lake effects. The winds aloft were weak -and variable as a high pr-essure ridge moved in over the area, Figures 15 - 20 and lower insert on Figure 11. No clouds were sighted near the eastern shore of the lake at any time during the day. The solar radiation measured at the Lake shore is presented in Figure 21. The total intergrated solar radiation for 25 June, 1965 was 672 cal cm - day, which is in good agreement with values given by CRREL (1964). The sun rose at 0506 and set at 2029 EST. -21 -

FRIDA2?f TTI,72:25, 19bt Maps propard by.National tI ito icCtr Wshingto, D: C. 170' 160, 150' 1,10' I-V )IV TD' 9C' 60' 7V 30' 125' 1 20- 155' 110' 105, 000 955 90. 85' 80.' 655'0'75 76 '/....~, N,4~ /,. 3oo ~o V'..o.......... NN.. _. ', '/ ' / b3< '3~ J ".., ~o05 4 4,. f 4 4'!\ qf...1-z.. ~-'..'..!-'01 ~o ' 9;0 6., L,%.~~~~~~~~~~~~~~~~~~~~...o.. 0..9,9.~ 6_ -10 9,9 ~4 ~.........5~N 009~~~~~~~~~~~~ ~.....OA f i-0 4y> ~.. y. 5 ~.~ h~~~,'eatr 16.49 4' 4y~ ~ ~ ~~~~~~~< / "49 99 Ctt~y,3; t 4,o~6 N ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~,t.-, ' iiJ~ '1 4,,~~; 0,,..~5 94994~~590o4..496 " 91" 4 " ' " Ix?,k-N\/II0y 0( Bay,.04 94'\ 3 "~~19 1\~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~J '%'~ 9."49, / t"%o~ 6419 6. 1410.......... / ~~~~~~44 ~~~~~ 06ao S ~ 10 N,~ ~ ~ ~ ~~~~ ~~~~~~~~~~~~~~~~~~~~~1 04o0 "1 "1 9..LJ4' LC -9 99 9 6 91 '/ 5400 a041 25-"' 9- l 491 \&" 500 MILLIOAO 00400"' 0007070' /0 __________________________________________ C654~~~~~~~~~~h9 C509t~~ 91' Surface Weather 414He ' 4 704PM 00:9000,: D..-;,,........ Juno 24... 1 M ~.;: 'l-. ft..: _ _ _ _ _) _: ___,...,,:.".00 eairDre' aiyWate a at.i 010.ST,:-~ 25 June,~ 196.1..:o SURFACE WEATHER AT~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ ~......:0 P.M.............. '\".T.,, YETRA 1-b- p-i 1... rI.Z... rH~~s!a ll ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~........ i. di.............i..s..i.::...:I:r -~ ho ighp -4 h 13ser EShw 'h e -eJune.isobar96at 130 EST.24Jun4ad teslwe irsert-s). ""1 t~Le.4e~ht conto~ ~or the 500 mb.e- sr c a 1 0, 2, e......... 12'.15.."""C " ' I'>' 85...,,....... '".. ' oe or..,,~,-..~~~~~~~~~~~~~,: Cit.....x.p::.'b''......4.~b.//... S~~~~~~~~~~~~~~~o...,-' —""'' AO en~~~~~~~~~~~L St Grand~~~~~~~~~~~~ "~;:~ ":'" r,,,, ~ ~, ~ ~~~~~~~~~~~~............. '" '.1: ~~~~~~~~~~~~~~~~~~6: o0~.',,.,..-.... ~on....,,.~!:'............~~~~~~~~.......:'~ ''.......~."';; '~~~~~~~~~~~~~~~~~~~ilwe. - ~- '\0:'~ 35~ ~ ~ ~ ~~~ ~~~~~~~~~~~~~~~. "u ~ 7.':,-d Roswell~:, offI~ ~ ~ ~~%, v....: z.r ----'.... ' I-Ls.,,+,- ',, r...,~' 3C ~ ' ~"", - ' 4........"..~,b-:.... ~,,~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~s,,.~....,. ~.~.-:-', x..... io":..':.' ~ '-,,'....'"'" ~ E~:~:.,.-~.-:~'~~i~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~puym, pu:' --.....,. '.....~~~~~~~~~~~~~~~~~~~~~~hiuau \..~,...... ~.~. '~~~~~~~~~~O,Christ ~~~Surface Weather 500-MILLIBAR ~ ~ ~ ~ ~ ~ 50m,EG'T COTOR AT 7:00.' P~?L.M "L.~%t~V[ ~~.,~ E, S.-t T~'' ~'_'-~~'.,''~ YETRA Ol0 EST June 25, 1965'x ' ~, \%, I'"',,'"'~:: '.'::... \;!q....nclva ev C —\ ~, 12' 120 i" f 0 11 ` 75'C.... FIGURE -11 U. Z'g, 'We a> I' — ho u aDiyWahrMa t00 S,2 ue 9 Upper i~nser~t shows tthe sea level=:- isobars at 1300 EST, 24 June and the lower Ja~isr so~,,7 -ileheahn~ conto....s for the 500 mb surface at 1900 EL-.T, 4-rn

-23 -73" 14 ~~~~~~~~~~~~~~~~~~~~~/z o Z,../u I,/~.15, 0 ~~~~~~~~~~~~~~~0 Es r JUNE25 o3 I, ~ ---=-,~.4 Ti. -—,,.~,r/~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~S 0 I 0~~~~~ ~ 0147) OFk/ 0~~~~~~~~~~~~~~~~~',",,/

-24 -10 It /goo Z i to /300 es 9 6-15' W TO 0 GREAT LAKES PLOTTING CHART 11 Q40 2 14 *0 1' Ti.. DO* (3 GLO A..Iyt 650,EI20 0 13 UM".'flty M Michig.. 2 D.pt..f M.t..,.I.gy..d 0 —g-phy r'. 0 'IO 0 0 1 0 0 0 IT 000'-..,. I zp- 4 00 O 4oo 9L.-t-0 viel&o) 0 EAy; 51.5- 01..144 -03 b 0 0 06 0 'Liss A'4 Oa,\ -r PA 0 0 0 0 LA..9 10. E%1 -0 AV.5 so Lo) I; Q-ov 0 41. 01: 0 ZT- 0 '5 03L 09 10 v I LAW... Is' is DA 0 xt - k-A L 7"Y 15 24 A 151 00 15+ 0Ell op 0 400/-O + "O.,41 0 rQ. 0 ICHIGAN -'\ INDIANA.0 0 P 10 Z-) z C,-,, 00,A 15 1 ' 0.3 2F,,6115 14 is L A /_0 v6 LAO'D 0 0 0 0 A. D. so -7 -0 ---------- 25 0 UI - 230 25 06 2.E. X4 A 0 0 9 I Pt C; %4 2 1.Al. 00 is 07 1\ IL 2 -114II D. Os T aw q eA env -.r FIGURE 13. mesoscale surface weather map and station weather at 1300 EST, 25 June, 1965.

-25 -~ ~~~~~~~~~~~~~~~~~~~~~~~~002 to (000 Z 6~~~~~~~~., 0~~~~~~~~~~~~/O $ MOO )~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~O ~s~~~~~~~~~~~~~~s 2~~~~~~~~~~~~~~1

,,~~~~~~~~~~~~~~~~~~~~~~~~~~~o,~~~~~~~~~~~~1 40'.. ~o,.""-'~'... """,, so~~~~~~~~~~~~~~~~~-" *'~~~~~~~~IT, /.XA lo. FIGUR 15. Heigt c nor o h 5 b sr ac t 10 S,2 ue 9 5 '.

.m~~~~~~~~~~~~~~~~i iI"~~ '~~~~~~~~~(4 ~'~.~,,~~::~~r?~~~~~49 0~~~~~~~~! 2.~~~~~~~~~~~~~~~~~~~~~~ /~':. '~~~~~~~~~ \~!~~~~~~~~~~~~~~~~~~~~A..'" ~. ~~'~~~~~~~~~~~~~~~~~~~~1,'~'"" ---~1, ~ ~. ~. //~~~~~2 "N,~~~~~~~~~~~~~~~~~~~~~~ ~~~~~~~~\ )c~~~~~~~~~~~e~V =Plz~~~~~~~~~~~~~~~~~. ~,,~>.V I..< % ~,% -.,_.., FIUE1.Hihotur. rte85 bsrae t00 S, 5Jn,16

00~~~~~~~0 10. 8SO~~~~~~~~~~~~~~~!3 N!C AU2AS ~~~~~~~~~~~~~~~~~~~~~~~~~~O.~~0 - L~~~~~~~~~~~~~~~~~~~~~~~~~~~~. ' — 'A %~~~~~ w FHnts 1900 ET, 2...ft__ ~/~~,~~~ 33~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~' RVNW 'fM M.% ru t FIGURE 17. Height contours for the 850 mb surface at 1900 EST, 25 June, 1965.~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~

V~~~~~~~~~~~~~~~~~~~~._ 1 71A, IPI ( ~ FU 1 H h o u f t 7 nsf a1 E 2 Je 9 4y-~~ ~ ~~ ~ ~~ ~ ~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~ ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~.o 8 '79 0~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~./.~~~~~~~~~~~~~C N.~ ~~~~~~~~~A ' I~~~~~~~~~~~~~~~~~~e k~~/ 16. 7001B!tic A 1M. ' U ~ on~~~~~~~~~~~~~~~~_. FIGURE 18. Height contours f or the 700 mb surf ace at 1900 EST '24, June, 1965.

'e ~ ~ ~ ~ ~ ~~~~~I J' ' -'~~~~~~~/X ~~~~~ '""'~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~(00P~~~~~~~.01 ~ ~ ~ ~ ~ / ' ~~~~ 720023 -S II?7., -I~~~~~~~~~~~~~~~~71 FIGURE 19~~~7. Heghontour fo th 70.bsufct 70ES,2-un,16. 00~~~~~~~~~~~~~~~~~~~~~~~~~~~":, v ~ ~~~~~~~~c ~.-. ~.~~~~~~~~~~~~~~~l \~~~~~~~~~~-,,,'...; '"' ~~~~~~~~~~~~~~~~~ 1?-0....:_....".-...o~ _ FIGUR 19.Heigt cotour forthe 0 0 bsraea 70 S,2 ue 95

'~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~' 'I,' I (I'.~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ FIGURE 20. Height contours or the 700 mb sufaceat1900ES 25June,1965 AK~~. ' ~ FIGURE '20. Height contours for the 700 mb surface at 1900 EST, 25 June, 1965.~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~.l

-32 -1.5 1.5 z -J0 1.0 0.5 0.5 0 0 04 08 12 16 20 TI ME (EST) FIGURE 21. Solar radiation recorded at the Lake shore station on 25 June, 1965.

4. OBSERVED TEMPERATURES, HUMIDITIES, AND WINDS This section includes graphical and written presentations of observed temporal and spatial variations of temperature, moisture, and windo 4.1 TEMPERATURE AND MOISTURE The lapse rates measured in the lowest 80 m at WJBL at various times are presented in Figure 22, together with the temperature profiles in the first meter of the soil. The data used for these plots are presented in Table A2. While the diurnal temperature fluctuation at 1 m depth was less than 1.2~C, the difference between maximum and minimum temperatures at the surface (1 cm below the surface) was 26o0~C. At all times the air temperature recorded at the 2.4 m level was lower than those recorded at the surface. The problem with correct measurement of the surface temperature is well recognized. The top soil is "penetrated by", and rapidly responds to solar heating, while the response to nocturnal cooling is slow and retarded by heat flux through the soil The nocturnal inversion was broken at sunrise. At 1300 EST a superadiabatic layer was present up to approximately 40 m. At 1600 EST the effect of the incoming lake breeze was seen in the lowering of the temperature in the lowest layers. The return to a nocturnal inversion condition after sunset was observed. In Figure 23, lapse rates obtained from airplane data are presented. The data used -33 -

-34 -80 - -80 ~ i ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~1. 60 1 60 r-. 0 O3 N. o Ia 40 I 4O 0:2 I-..I -0.... I I 'z!0-2 II ',t / / ~0 0 6 0P. 5 10 15 20 25 30 TEMPERATURE IN C FIGURE 22. Lapse rates and soil temperature as a function of time at WJBL tower on 25 June, 1965. Times indicated in Figure are EST.

2500 2500 LAKE LAND LAKE LAND LAKE LAND 0800 0850 1015 1100 1300 1350 2000 2000 1500 — QI 5 1 15001 %~~~~~~~~~~~~~~ r'r'~ ~ zd a I~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ 5000 500 500~~~~~~~~~~~~~~~~~~~~~~~~~5 5'~ ~~5 0 I 5 I0 15 5 10 15 5 10 15 5 10 15 5 10 15 5 10 15 20 TEMPERATURE IN ~C FIGURE 23. Lapse rates over lake and over land at various times on 25 June, 1965.

-36 -in the presentation are tabulated in Table A3. The airplanes ascended over the lake at x = -32 krm, y = 0 km and decended over land at x = 32 kmin, y = 0 km. The times for the beginning of the ascent and descent are given on the figure. While the air over land assumed near adiabatic lapse rate below 1500 m in the early afternoon, the air over the lake remained relatively stable in response to the colder surface water and subsidence due to the lake breeze circulation. Vertical temperature cross sections along the observation line are presented in Figures 24-26. In order that data collected at and near the surface could be used, a logarithmic height scale is used. The data used for the Figures are tabulated in Tables Al-A3. Figures 24-26 illustrate how the air over land was warmed and that the air temperature over the lake changed very little. It should be noted that a horizontal temperature gradient across the shoreline of approximately 1.2kC kl1 (6 C in 5 km)had been formed in the early afternoon. Figure 27 presents temperatures as a function of time at various stations and at various distances from shore, as well as water temperatures recorded onboard MYSIS.

3000 UP 0800-0824 1 ~6 ~ I I DOWN 0850-0908 2000~ 6 8~~~~~~~~~~~~~~~~~~ 12 500 - 14 ----"t 12 F- 0737 ~ 100 '50 44 10 -40 -30 -20 -10 0 10 20 30 40 LAK E LAND DISTANCE INLAND IN KM FIGURE 24. Analyzed vertical temperature field in early morning, 0737-0908 EST, 25 June, 1965. Note that a log-scale is used for the ordinate to allow surface and tower data to be illustrated as well as data obtained from further aloft by aircraft.

3000 UP 1016-1037 66 DOWN 1103-1121 20001 8 r I r _ 8 10 5000 14 -- 16 CT ~~~~~~~~~~~~~~0953 Wt 16 X0100 z H 17 cD c 50 17 _____ _18 1 18 10 -40 -30 -20 -10 0 10 20 30 40 LAKE LAND DISTANCE INLAND IN KM FIGURE 25. Analyzed vertical temperature field in late morning, 0953-1121 EST, 25 June, 1965. Note that a log-scale is used for the ordinate to allow surface and tower data to be illustrated as well as data obtained from further aloft by aircraft.D

3000 I I U P 1256-1317 DOWN 1345 -1404 8 1 A} --- — - -- 20 0 0 -FIGUR 26-. ----edvricltmprtrefed-n-rl-feron 12 LO 500 14 -z 16 16-"' " " 1 ' 100 20 50 ~~~~10~16 - 40 -30 -20 -10 10 I2 30 40 LAKE LAND DISTANCE INLAND IN KM FIGURE 26. Analyzed vertical temperature field in early afternoon, 1232-1404 EST, 25 June, 1965. Note that a log-scale is used for the ordinate to allow surface and tower data to be illustrated as well as data obtained from further aloft by aircraft.

LAKE BREEZE AT Shore 6 KM 8 KM 16 KM 0 KM 25- -25 20-,m ru 20 o d 15 from s15 md MKG(6KM)....... " MYSIS AITER TEMP_________ t M wed1 MYSIS WATER TEMPm Wu Shore. 1 0 - 24KMl-*-*- 10 8KM \ PORT DL6.4A 1.6 6.4 1.6.4 PORT -_ _.8 PORT VPOSITION OF MYSIS IN KM OFF SHORE 5 15 5 00 04 08 12 16 20 24 TIME (EST) FIGURE 27. Temperature as a function of time at various stations and various distances from shore on 25 June, 1965. Included are air and water temperatures measured from the MYSIS at indicated distances off shore. Air temperatures onboard the MYSIS were sensed 11.8 m above the lake surface while the water temperatures were sensed 1.2 m below the lake surface.

-41 -The data are tabulated in Table Al. The "heating curved" for the 24 km station agrees within + 1 C with the one observed at GRR, 53 km inland, indicating that the lake breeze never penetrated as far as 24 km.o- The "heating curve" measured at the 2.4 m level at WJBL, 10 km inland, is in close agreement with the one observed for the 8 km station. Local environmental differences seemed to effect the night-time values of temperature at the stations: however, the daily heating before lake breeze penetration was similar at all stations. When the cold lake air was brought inland by the lake breeze and reached a station, a definite drop in temperature was observed. The times at which the lake breeze reached the various stations are indicated with vertical lines in the figure. Changes in the air temperature over the lake indicate, that before approximately 0900 EST air was flowing off land, reaching at least 1o6 km off shore. Similarily, in the evening the onset of a land breeze was noted. Comparison of air and water temperatures recorded onboard MYSIS with those air temperatures recorded elsewhere suggests the existence of a dome of cold and stable air near the water surface

-42 -It should be noted that the water temperature was varying with time of day and distance from shore, the "day heating" observed.'being approximately 1.5 C both at 1.6 and 6.4 km off shore, while the water was on the average 1~- 2~C warmer at 6.4 than at 1.6 km off shore. Although the difficulties in obtaining accurate measurements of moisture parameters are well recognized some analyses of the moisture structure was attempted. The dew point temperature as a function of time at various stations is plotted in Figure 28 and tabulated in Table Al. As the colder and more humid lake air moved inland with the lake breeze, sudden increases.in dew point temperature were observed at a station. The time of lake breeze penetration determined by "dew point increase" is in excellent agreement with the time determined on the basis of "temperature drop". Dry bulb temperatures and, to a lesser degree, dew point temperature observed at the inland stations and compared with observations at the lake shore and onboard the MYSIS indicate intense modification of the lake air in a short trajectory over land. Due to a lack of confidence regarding the time constant and accuracy of the airplane moisture measurements, no vertical cross section of moisture structure is presented.

15 15 LAKE BREEZE AT Shore 6KM 8KM 16KM O 0KM 0 o~~~~~~~~~~ */ /0 SHORE I6KM -MYSIS 6KM(MKG) K G<.>Y 4 10 -x; MYSIS A 4~~~~~~~~v~~~~~~~~s "~~~~~~001N Uj lii 5 - _______~~~~~_____,_.i // --- PORT 1.6 6.61 <.6 64.4 PORT 1.8 PORT I 1 1 11 -- I --- POSITION OF MYSIS 2INKM OFFMSHR 00 04 08 12 16 20 TIME (EST) FIGURE 28. Dew Point temperature as a function of time at various stations uJ. and various distances from shore on 25 June, 1965. Included are dew point POSIIONOF YSI 24NKM F HR adaiu itne r so o 5 Jue 95 Icue r w on temperatures measured from the MYSIS at indicated distances off shore. The sensor onboard the MYSIS was located 5.0 m above the lake surface.

4.2 THE LAKE AND LAND BREEZE CIRCULATION The extensive measurements of the circulation, that were made along the observation line and elsewhere in the neighborhood of that line, are presented in tabular form in Tables A4 and A5. In addition to the total wind (VT) and the wind direction (WD), the across-shore component (U), positive inland along the positive x-direction, the along-shore component (V), positive toward the north along the positive y-axis and in the cases of double theodolite tracking, the vertical wind (W), positive upward along the positive z-axis are given. Isotachs for the U and V components are analysed for 0830,1100, 1400, 1700 and 1900 EST and presented in Figures 29-38. In order that the details near the surface could be included, a logarithmic vertical scale is used. Vertical profiles of the Ucomponent at various times and at the various stations are presented in Figure 39. Figure 40 presents temporal variations of the wind in the land, lake, land breeze circulation at various stations. The black arrows indicate surface, or near surface winds, the red arrows indicate the 200 m winds and the blue arrows indicate 1050 m winds. The maximum lake breeze, an onshore -44 -

-45 -4000 4 -I 2000 100 - FIGURE 29. Isotachs for the across-shore component ) at 0830 EST, 25 June, 1965. Positive values, Wind speeds are in m s -10 LAKE -5 0 5 LAND-10 15 20

4000 -I111 l-I -9 -9 2000 -7:5 -5 -. 1000 -5 w -- I I - - ' 100 ~~~~~~~~50 I00 2 _ -I l -10 -5 5 10 15 20 LAKE LAND DISTANCE INLAND IN KM FIGURE 30. Isotachs for the along-shore component (V) at 0830 EST, 25 June, 1965. Positive values, hatched areas, indicate southerly winds and negative values indicate northerly winds. Wind speeds are in m sec-1

-47 -4000 -4 -4 -4! -4 4 2000- - - 4 -2 2 -500 -3 --2 I 100 I' ~ ~~- "D~~ -10 -5 5 10 15 20 LA KE LAND DISTANCE INLAND IN KM FIGURE 31. Isotachs for the across-shore component (U) at 1100 EST, 25 June, 1965. Positive values, hatched areas, indicate westerly winds (onshore) and negative values indicate easterly winds (offshore). Wind speeds are in m sec'1.

-48 -4000 -8~ - 8 -6 -6 -4 — 4 2000 - - -- -3 1000 -2 -3 -2 500 0 U) w /~~~~~~ cc ~z Ir I 100 I 50 -I -I ~~~~~~~~~~~Pf~~~~10~~~~~~~~~~ I::r..__ _ __ __ __ _ ___ _ _ _ _ _ _ _ _;/I { 11 -10 -5 0) 5 10 15 20 LAKE LAND DISTANCE INLAND IN KM FIGURE 32.' Isotachs for the along-shore component (V) at 1100 EST, 25 June, 1965. Positive values, hatched areas, indicate southerly winds and negative values indicates northerly winds. Wind speeds are in m sec-l

-49 - 3000 -- 3 -2000-3 - 3 1000 15 20 Wr 500 --2 DISTANCE INLAND IN KM FIGURE 33. Isotachs for across-shore component (U) at 1400 EST, 25 June, 1965. Positive values, hatched areas, indicate westerly winds (onshore) and negative values indicate easterly winds (offshore). Wind speeds are in m sec.

-50 -4000 3000- -4 0 2000 - 100 - 0 /, _w~~~ -I ~__.2~2 Un 500 -_1 W -I-2 W F-~~~- IDISTANCE IN LAND IN KM.50 - 3 ~~~~~~~~-2 lot__ -3 2I -3 -2 -10 -5 5 0 15 20 LAKE LAND DISTANCE IN LAND IN KM FIGURE 34. Isotachs for the along-shore component (V) at 1400 EST, 25 June, 1965. Positive values, hatched areas, indicate southerly winds and negative values indicate northerly winds. Wind speeds are in m sec-1.

-51 -2000 I OO- I 3000 -I -2000 2 2 -2 5000 -4 -3 -500 OI 2~ -10 5 5 1 0 15 20 LAK E LAND DISTANCE INLAND IN KM FIGURE 35. Isotachs for the across-shore component (U) at 1700 EST, 25 June, 1965. Positive values, hatched areas, indicate westerly winds (onshore) and negative values indicate easterly winds (offshore). Wind speeds are in m sec-1.

-52 -4000 3000 2000 D 1000 0 500 - lo L 143-rvv02|/,og, LU w -2 -3 Z -4 z I00 50 3 0,o 3, o A o -10 -5 0 5 10 15 20 LAKE LAND DISTANCE INLAND IN KM FIGURE 36. Isotachs for the along-shore component (V) at 1700 EST, 25 June, 1965. Positive values, hatched areas, indicate southerly winds and negative values indicate northerly winds. Wind speeds are in m sec-1.

-53 -4000 2 / I -I 1000 -4 -3"-3 -4 in ec500 -1 -r, 50 -10 -5 5 10 15 20 LAKE LAND DISTANCE INLAND IN KM FIGURE 37. Isotachs for the across-shore component (U) at 1900 EST, 25 June, 1965. Positive values, hatched areas, indicate westerly winds (onshore) and negative values indicate easterly winds (offshore). Wind speeds in m sec-1.

-54 -4000 3000 -I O -2 2000 3 1000- 0 500 C) -I Wz ~- -2 I00 50,0 ~~~-10 -5,5 10 15 20 LAKE LAND DISTANCE INLAND IN KM FIGURE 38. Isotachs for the along-shore component (V) at 1900 EST, 25 June, 1965. Positive values, hatched area, indicate southerly winds and negative values indicate northly winds. Wind speeds are in m sec-l

LAKE 1203X =-1.3 MYSIS SHORE 8 KM 16 KM 2500 / ~~~~~~~~~~~~~~~ oo./..?.:~.~/ / \ I 1347, X -6.4 \ ~ ~ ~ ~ \b?' 2000 I/.~~~~~~~~~~~~1 ' Cl)~~~~~~~~~~, w~~~~~~~~~~~~ Cn 0D z CI-) I - - 5' U' = oo =t a i~~~~~~~~~~~~~ 1000 500 '~ 09021203 \1900 100 \190 0 I 137\Il o? r 93 OJ I ~ ~~~~~~~ ' 500;'\I, /~~~~~~~~~~~~~~~~~~~~~~ 0 Q63',,,,,o,2~3 17 I OiC 00 -8 -4 4 -4 0 4 -8 -4 0 4 -8 -4 0 4-8 WIND SPEED IN METERS PER SECOND FIGURE 39. Across shore wind component (U) as a function of height at various times and stations, 25 June, 1965. Times given in figure are EST and x-values given for MYSIS indicate the distance off shore in km.

~uy 1o[ UT aqs 3Jo ou~4syp a$e;ypuT jIopeoa,SISAW spyseq qcwnN 'S96T 'eun~ f Z,suoTqps snoTIA qp pup seuiTq SnOTaPA 4 4oIP u0 Q~0I pue ui 00Q 'leojpns 9l q 4 SaO4SA PUTM '0.IfDI. l9 S91 INN 8 (N 9 30 9' - SISiN _z - 0- 91, - 91 ~~~~~~~~~~~~ VI- t;_.9. VI.~.,,., ~ ~ — - -....L I ~s 9.1 -91 -01 - 81 -r t ~ tx ---e~~ '1 ~ o 91 -90 0 01Z 0 VY 003 z - 8'' 3 ovi 8 n s ooz 300Tfl-JSJ 91-,__., 90 3 ~~~~~~~~3S.9 -_ /. ~ '.,~.~~~9~i

-57 -wind, and the maximum land breeze, an offshore wind were observed, at about 200 m. The 1050 m level was chosen to be representative of the return flow, the offshore wind aloft in the lake breeze circulation. There was some indication of a return flow associated with the land breeze circulation, in this case an onshore wind aloft with a maximum in a layer above 1200 m; thus not truly represented in Figure 40. The data tabulated in the appendices contain information that has been left out in the graphical presentation, and has been included only partly in the verbal description of the circulation. As can be seen from Table 1, winds aloft data are available for every 30 minutes near the shore between 0600 EST and 2030 EST. A total of 62 pibal measurements were made and half of these observations were by double theodolite technique and analyzed for vertical velocities as well as for horizontal winds. The low level land breeze observed at all stations in the morning was reversed to a lake -breeze at various times during the day and then again reversed to a land breeze in the early evening. The times for reversal to a lake breeze are in close agreement with the times at which the lake breeze could be

-58 -detected at the respective stations, on the basis of temperature and dew point changes, Table 2. Between 0600 EST and 0700 EST a maximum land breeze was measured at the 8 km station, at the shore and from the MYSIS stationed 1.6 km off shore. A maximum wind of 8 m sec was observed at 180 m and the depth of the offshore flow layer was more than 1000 m. There was some indication of a return flow layer, or at least of a return flow effect above the land breeze. Below 400 m, at the shore, subsidence,, with a maximum downward velocity of 21 cm sec-1 at 265 m, was observed. Upward velocities were found between 400 m -1 and 2000 m, with a maximum of 82 cm sec at -1 1700 m and a secondary maximum of 49 cm sec at 560 m. At 0830 EST the land breeze had a maximum -1 offshore wind component of 6 m sec at 300 m at the shore. The depth of the offshore flow layer was still about 1000 m. An onshore flow layer above 1000 m near the shore suggested a return flow in the land breeze circulation. A southerly wind component observed near the surface over land was evidence of a Coriolis effect on the land breeze, while a northerly gradient flow aloft masked any such effect

TABLE 2. Local times for lake breeze frontal passage at various stations as detected in wind direction change, temperature drop and dew point rise near the surface on 25 June, 1965. The time selected is the time when a change began to take place. The value in bracket is the change that was observed in the next half hour in degrees and OC. For the lake shore the wind change at 200 m is given and for WJBL the wind change at 20 m is given0 For MKG and WJBL half the subsequent one hour change is givSi.1 STATION MYSIS LAKE TOWER LAKE SHORE MKG 8 KM 'WJBL 16 KM X-distance -6.4 km -1.6 km 0 km 6 km 8 km 10 km 16 km WIND DIR. 1030(200) 1000(130) 1100(90) 1300(65) 1530 (180) 1600(110) 1830(160) TEMPERATURE 1030(0.7) 1130(1.1) 1300(0.6) 1600(1.7) 1630(0.9) 1800(1.1) DEW POINT 1030(1.6) 1100(3.9) 1300(1.7) 1530(2.2) 18000.9)

-60 -in the return flowo An average ascent was observed at the shore, with a maximum upward velocity of 97 cm sec-1 at 1600 m and a secondary maximum of 37 cm sec1 at 500 m. Between 0900 EST and 1100 EST strong upward currents were observed near the shore in -1 the lower 1000n-m A maximum of 262 cm sec was measured at 1000 EST at 455 m and an average upward velocity below 1000 m between 1000 EST and 1100 EST of 146 cm sec-1, was observed. At 0900 EST an onshore wind component of 1.4 m sec-1 was observed at 1280 m 2.4 km off shore. At 1100 EST an offshore wind ex-l ceeding 0.7 m sec was observed at that level 7.4 km -off shore -and at 1200 EST the wind at 1250 m at 2 km off shore had increased to -1 5.3 m sec and with an off shore direction. Closer to shore the wind had an onshore component at 0930 EST in a layer between 1250 m and 1650 m. At 1000 EST the wind in that layer had an offshore component and at 1100 EST this offshore wind component showed a maximum -1 of 2.1 m sec at 1290 m. At 0900 EST the onshore wind component at 7.5 km inland exceeded 1 m sec 1 in a layer between 1150 m and 1500 m. At 1100 EST the wind in that layer had a maximum offshore component of -1 2.3 m sec at 1500 m.

-61 -Both over land and over water there was a direction change toward more offshore wind in a layer between 500 m and 2500 m between 0900 EST and 1100 EST. At the surface the land breeze was weakening. At 1030 EST a windshift from land to lake breeze was observed at the Lake tower, 1.6 km off shore, the MYSIS, then at 6.4 km off shore reported calm conditions. At 1100 EST an onshore surface lake breeze was observed 6.4 km off shore. At 1130 EST the lake breeze reached the shoreo A maximum onshore component over the -1 lake of more than 4 m sec was observed from MYSIS at noon, near the surface at 1.3 km off shoreo The depth of this onshore flow layer was 350 m and a downward velocity in that layer of 25 cm sec at 160 m was observedo In the layer between 350 m and 1700 m the air was in general ascending with a maximum of 67 cm sec at 865 mo At 1400 EST the return flow layer had its maximum offshore component of more than -1 5 m sec at 1200 m at the shore and over the lakeo The lake breeze had reached 6 km inland, had a maximum onshore wind component of 3 m sec 1 and a depth of more than 300 m at the shore. Inland from the

-62 -lake breeze front (the convergence zone), the wind was from the south-easto Above the shore a general ascending motion was observed in the -1 lowest 1300 m, with a maximum of 76 cm sec at 890 m and a secondary maximum of 28 cm sec at 400 m. Near the lake breeze front the up-1 ward velocity was 100 cm sec at 120 m, -1 with another maximum of 400 cm sec at 1350 m. The Coriolis effect was recognized both in the onshore flow and in the return flow of the lake breeze circulationo At 1700 EST the lake breeze had reached about 12 km inland, had a maximum onshore -1 wind component of more than 4 m sec at 100 m over land and a depth of 300 m. A maximum offshore wind component in the return flow of more than 5 m sec was observed at 1450 m at the shore. The vertical wind was upward in the lowest 650 m above the 8 km -l station with a maximum of 55 cm sec at 500 m, and had a strong downward component of 88 cm -1 sec at 750 m. The Coriolis effect was again apparent, giving a northwesterly lake breeze flow and an overriding southeasterly return flow. At 1900 EST the lake breeze was '"dying'" near the shore leaving only a 3 m sec northerly component at the surface. At 16 km

-63 -the wind was still off the lake with a speed -1 of 3.2 m sec at 90 m. The wind at 1000 m was from the east, with a speed of more than 5 m sec. The vertical velocity was in general negative in the lowest 1200 m, with a maximum downward motion of 170 cm sec, observed at 1200 m above the 8 km station. Only in the first 100 m was a slight upward motion of less -1 than 25 cm sec observed. Between 1930 EST and 2100 EST the lake shore station as well as both the inland stations and the off shore station showed a reversal to a land breeze near the surface. At 2030 EST both the 8 km and the 16 km stations showed calm. There was some evidence of a return flow, associated with the onset of the land breeze circulation in a layer between 1600 m and 2400 m. It should be noted that upward vertical velocities exceeding 100 cm sec -1 were commonly observed near the lake breeze front in the lower 1100 m where maximum values exceeded 200 cm sec-1. Before the arrival of the front at the 8 km station, the flow was very unstable with vertical velocity variations -l -1 between +100 cm sec and -100 cm sec in the lower 1000 m. After the passage of the lake breeze front the flow 'seemed to stabilize.

-64 -Both at the shore and at the 8 km station the vertical velocities were upward in the lake breeze onshore flow, but in general less than -1 50 cm sec Above the lake breeze, in the return flow layer, the vertical velocities at the 8 km station indicated convergence at about 700 ma while at the shore a general ascent, with upward motions exceeding -1 70 cm sec was observed up to 40.QQ00 m Observational errors gave some extreme values, -1 but vertical velocities of about 400 cm sec appear to be real. A general subsidence, with downward velocities of less than 30 cm sec was observed in the lower 1000 m in the evening, after the reversal from lake to land breeze. Qualitative observations, i.e. traces of recorded winds and temperatures, indicated that the lake breeze front penetrated inland in a series of pulses with a period of less than 2 hours.

4.3 SUMMARY The spatial and temporal variations of temperature, moisture and wind near the eastern shore of Lake Michigan have been observed and described for 25 June, 1965. During this day a weak northerly gradient flow prevailed and a well developed lake breeze occurred. In summary the observations show: 1. The effect of the differential heating between land and lake surfaces led to a strong horizontal temperature gradient near the surface exceeding 1.2~C km (60C/5 km) across the shore in the afternoon; 2. The temperature of the air over land became equal to the temperature of the air over the water and also to the lake water temperature between 0700 EST and 0800 EST and again between 2000 EST and 2100 EST; 3. Air over the lake remained relatively stable throughout the day in the lowest 600 m. Intense modification of this air in short trajectories over land was observed. Intense vertical mixing led to adiabatic and even superadiabatic conditions over land -65 -

-66 -in the afternoon. Strong nocturnal inversion over land in the lowest 80 m was observed.. Isothermal conditions in that layer occured at about 0730 EST and 2030 EST; 4. An offshore flow aloft, the return flow, was observed at the shore in a layer between 500 m and 2000 m between 0800 EST and 1100 EST. This observation was the first indication of a lake breeze circulation; 5. The onset of an onshore flow, the lake breeze, was observed near the surface over the lake and at the shore between 1100 EST and 1130 EST; 6. While the return flow, once established, seemed to be steady, qualitative observations indicated that the lake breeze penetrated inland in a series of pulses with a period of less than 2 hours; 7. Strong vertical upward motion exceeding -AL 200 cm sec, coupled with low level horizontal convergence, occurred near the lake breeze front, the

-67 -lakeward sloping surface between the advancing cooler air off the lake, and the heated air over land. Air temperature drops of more than 1 C, dew point increases exceeding 3 C, and reversal of surface winds occurred within one hour, as the lake breeze front passed. These changes were less pronounced the further inland the front penetrated; 8. The maximum depth of the layer of onshore flow was 400 m near the lake breeze front in the late afternoon; 9. The maximum onshore wind of more than 4 m sec occurred in a layer 100-200 m aloft, immediately inland from the shore in the late afternoon; 10. Upward motion, in general less than 50 cm sec, was observed in the lake breeze flow layer over land, Downward motion was observed in that layer 1.2 km off shore; 11o The return flow layer aloft was more than 2000 m thick at the shore, with a maximum offshore wind component in excess of 5 m sec

-68 -at 1200 m in the late afternoon; 12. The vertical velocity varied from -1 -1 +70 cm sec to -70 cm sec in the return flow layer. Several vertical convergence layers were observed with the most pronounced at about 700 m near the lake breeze front; 13. The effect of the Coriolis force was pronounced in the onshore flow at about 200 m, but also noted in the return flow aloft. In the afternoon the return flow was from the east-south-east and sandwiched between a northwesterly low level onshore flow and a weak northerly gradient flow above 2500 m; 14. The maximum inland penetration of the lake breeze front was approximately 20 kmn, occurring in the early evening, when the low level winds near and off the shore already had reversed to a land breeze; 15. Although no definitive criteria were found to determine the depth of penetration of the lake breeze circulation into the atmosphere,

-69 -there were indications of influence in the flow pattern up to and above 4000 m in the afternoont 16. A low level offshore flow, the land breeze, was observed in the morning and again in the evening; 17. The depth of the land breeze was more than 600 m and its strongest offshore wind component of 7 m sec 1 was observed both. over land and over the lake at 200 m between 0600 EST and 0700 EST; 180 There was some evidence of a return flow associated with the land breeze circulation in a layer between 1200 m and 2400 m; 19. The effect -of Coriolis force was observed in.the land breeze circulation and was most pronounced in the lower layer of the land breeze. It was masked aloft by the -gradient flow; 20~ Shoreline downwash and upwash effects, caused by changes in roughness between land and lake surfaces were

-70 -apparent, i.eo the air in the land breeze layer descended as it moved across the shore and out over the lake, while the air in the lake breeze layer ascended at the shoreline, before any thermal instability was expected to have been induced in the layer; 21. Temporal and spacial variations of the water temperature in response to solar heating and dynamic air-sea interaction exceeded 3~C; 22. A mesoscale "lake high" developed during the day in response to the low level divergence and the subsidence over the lake and reached maximum intensity of more than 4 millibars in the early evening; 23. Surface wind data from stations around the lake suggested that the lake effect was homogenous along the lake shore.

5. A COMPREHENSIVE SUMMARY OF PREVIOUSLY REPORTED OBSERVATIONAL STUDIES OF LAND, LAKE, AND SEA BREEZE CIRCULATIONS. The observations presented in the previous section constitute, to the authors knowledge, the most extensive measurements of a landlake breeze circulation. It is evident that differences in the synoptic situation and coastal characteristics would influence observed circulations. The observations reported by Moroz (1965, 1967) under similar synoptic situations and at the same location are indeed in very close agreement with those reported here. His observations showed that the onshore flow in the lake breeze circulation, in general, had a depth of less than 600 m and that a maximum onshore velocity of more than 4 m sec occurred within 250 m of the surface immediately inland from the shore. Furthermore the return flow layer aloft was more than 1500 m thick and a maximum offshore velocity exceeding 3 m sec occurred in the afternoon at 1200 m at the shore. The depth of the offshore flow, the land breeze8 seemed to exceed 1500 m at 0900 EST on 23 July. 1964, and would have obscured the onset of the return flow in the late mornings there was, however, an -7L

-72 -increase in the offshore velocity at 900 m at the shore between 0900 EST and 1100 EST. The lake breeze onshore component was first observed at the shore at 1100 EST. At 0745 EST on 10 July 1963, Moroz observed a weak land breeze in the lowest 200 m 5 km off shore with indications of an overriding return flow in the land breeze circulationo Later that day at 1710 EST he observed a -1 2 m sec lake breeze in the lowest 200 m and an overriding return flow at more than 16 km off shore. The effects of Coriolis force were clearly evident both in the onshore and in the offshore component of the lake breeze circulation. Moroz found the lake breeze front to penetrate inland in a pulsating manner and that the lake air was modified after short trajectories over land. Observations reported by Strong (1968) were made on the western shore of Lake Michigan under essentially non-zero gradient wind conditions. Strong used single theodolite tracking of pibals in determining horizontal wind fields aloft. He calculated horizontal divergence and was thus able to evaluate vertical velocities. Upward velocities of -1 more than 60 cm sec were estimated 2.2 km inland and downward velocities exceeding

-73 -60 cm sec were found in the vicinity of 800 -1000 m at 2.2 km off shore. Lyons (1966, 1967) reported on lake breezes in the southern basin of Lake Michigan. He evaluated satellite cloud photos and compared them with cloud and smoke photos taken from the surface and from an airplane. A ring of towering cumulus associated with the lake breeze front was observed around the lake, suggesting along-shore homogenity in the lake breeze circulation around the lakeo The tops of these convective clouds were observed to be carried toward the lake in the return flow above the lake breeze and to dissipate near the lake shore. Lyons suggested that this dissipation was due to an increased stability in the lower layer, the lake breeze layer, over the lake and near the lake shore, thus a decreased convection coupled with a gravity type wave motion causing intense subsidence in the return flow layer. Subsidence over the lake was observed as smoke was carried off shore Aby the return flow aloft and was also evident from the lack of clouds over the lake itself. Chagnon (1967) and Lansing (1965) reported on average precipitation over the lake

-74 -and showed -it to be considerably less than over adjacent land areas. Lansing (1965) observed average temperatures over land to be more than 1~C higher than over water during summer months. Average maximum temperatures were about 40~C higher. Lyons observed lake effects in cloud layers 5000 m aloft. He also reported on meteorological observations made in the Chicago, Ill., area. He also observed lake breezes to penetrate more than 60 km inland and the depth of the lake breeze to be approximately 300 m. At one time on 7 June, 1963, the air temperature inland was more than 15~C higher than at the shore. The onshore wind component of the lake breeze was in general less than -1 5 m sec. It should be noted that the urban heat island effect and increased surface roughness has to be considered in the evaluation of these observations. Strong and Bellaire (1967) observed the onset of the lake breeze to be at the lakeshore and a subsequent growth of the lake breeze circulation cell both lakeward and landward. Hall (1954) summarized the synoptic conditions under which a lake breeze penetration 12 km inland, to Chicago Midway Airport occurred. He stated that, if the gradient wind is less -1 than 7 m sec with an along shore or offshore direction, the cloudiness is less than 6 tenths

-75 -and the air temperature is more than 5 C above the lake water temperature one could expect the lake breeze front to reach the airport in the afternoon. Reduced visibility at the airport could be expected, as the smoke filled convergence zone, the lake breeze front, reaches the airport~ He also indicated the occurrence of a lake high developing on lake breeze days. Defant (1951) gave an example from the Baltic sea, where the afternoon pressure on twenty sea breeze days averaged 0.8 mb higher on a lightship than at a land station. Hewson et al (1961, 1963) measured the natural ventilation on the western shore of Lake Erie and on the eastern shore of Lake Michigan. They found lake and land breezes to be frequent in the summer half of the year. Shallow lake breeze inversions were observed near the shore in the onshore flow. The depth of these inversion layers were less than 50 m and the inversions were found to be destroyed within 3 km from the lake shore. Munn and Richard (1964) observed land and lake breeze circulations on the eastern shore of Lake Huron under light gradient winds. They found the depth of the stable onshore flow layer to be less than 200 m at the shore and a new internal boundary layer to develop

over land in response to land heating. The depth of that superadiabatic layer was between 30 and 60 m at 300 m from the lake. The lake breeze was observed at the shore at about 0900 EST when a 1800 wind shift and a 30C temperature drop occurred. At about 1600 EST the lake breeze front was observed as a wind shift at 19 km inland. The temperature drop was more gradual and indicated intense modification of the air as it passed over land. Munn and Richards stated that this modification sometimes is so strong that the lake breeze disappears completely, permitting a new lake breeze front to form and move inland, Sea breeze observations reported by Fisher (1960), and by Frizzola and Fisher (1963) were made under essentially non-zero gradient wind conditions on the coast of New England. They found that the onshore flow of the sea breeze circulation had a depth of less than 1000 m at the shore and that the maximum onshore velocity occurred below 300 m near the shore in the afternoon. They also found that the depth of the onshore flow was greater when onshore gradient flow existed than with offshore gradient flow. The sea breeze front was more pronounced in offshore gradient flow

-77 -cases. The Coriolis effect as well as the return flow layer could be detected but were obscured by overriding gradient flow. Pack and Angell (1963), Angell and Pack (1965) and Hass et al (1967) observed sea breezes by means of tetroons and found that the onset of the onshore flow occurred 9 km off shore at 150 m, approximately an hour before the onset was observed at the shore. Furthermore, they found that the tetroon sometimes traced a small anticyclonic loop over the ocean before being carried inland by the sea breeze. Wallington (1959, 1965) observed average upward velocities of 250 cm sec-1 and occasional updrafts of about 800 cm sec in a sea breeze front. The front, sometimes less than 250 m wide was well marked by "curtains of clouds". Craig et al (1945) gave what has been considered a typical cross section of moisture in the sea breeze circulation. A dry tongue aloft, at about 200 m, over the water has been associated with the return flow aloft and the subsidence off shore. Atlas (1960) observed the sea breeze penetration by means of radar and suggested sharp moisture contrasts across the sea breeze front. He found moisture pick up to occur from the warm waters close to shore and to be most marked in air which had

-78 -a previous over land history, e.go land breeze air. Eddy (1966) observed the sea breeze to penetrate approximately 40 km inland from the coast of Texas and the land breeze to extend about 15 km off shore. He found evidence of diurnal wind variations at altitudes as high as 5000 m. Dixit and Nicholson (1964) observed the sea breeze near Bombay, India to extend more than 160 km off shore. They found the depth of the onshore flow layer to be less than 1400 m and some evidence of a return flow above that layer. Wexler (1946) reported on the land breeze over Lake Constance converging toward the center of the lake, with accompaning rising motion which caused stratus to form at about 200 m. This occurred frequently in spring and fall, but seldom in the summer. He also reported that land breeze fronts in the tropics may be locus of nocturnal cumulus and thunder storms. Wexler (1946) and Defant (1951) reported that the highest probability for lake (sea) breezes to occur is in the spring and summer, while land breezes are most frequent in the fall. They also reported that along coasts at middle latitudes lake (sea) breezes occur on more than 30% of the days in spring and summer. At higher latitudes the

-79 -frequency of occurrence is lower, e.g. at the shore of the Baltic sea, sea breezes are not expected to occur on more than 20% of the days, even in the summer. In the polar regions the phenomenon disappears almost completely. On tropical coasts the land and sea breezes occur almost ever day in the summer months, while they appear on about 30% of the days during the rest of the year.

6. CONCLUSIONS The "ideal" thermal circulations caused by differential heating and cooling of land and water surfaces are difficult to observe. Local climatological and topographical effects as well as non-zero large scale gradient winds influence the observed land and lake (sea) breeze circulations. The dimensions of these circulations as well as the magnitude of associated wind velocities, wind direction changes, temperature changes and moisture variations vary with latitude and horizontal extent of land and water surfaces. The reported observations give some guidelines to the search for a better physical understanding of how these circulations are initiated and how they develop. -80 -

REFERENCES Angell, J.Ko and D.H. Packo 1965. A study of the sea breeze at Atlantic City, N.J. using Tetroons as Lagrangian tracers. Mon. Weatho Rev., 93; 475-493. Atlas, Do, 1960. Radar detection of the sea breeze. J. of Met., 17; 244-258. Changnon, S. Ao, Jr., 1967. Average precipitation on Lake Michigan. Proc. 10th Conf. on Great Lakes Res., Int. Assoc. Great Lakes Res., Ann Arbor; 171-185. Craig, R. Ao, I. Katz,and P. J. Harney, 1945. Sea breeze cross sections from psychrometric measurements. Bull. Am. Met. Soc., 26; 405-410. CRREL, 1964. Daily sums of Global radiation for cloudless skies. Res. Rep. 160, U.S. Army Material Command, Cold Regions Research & Engineering Laboratory, Hanover, No H. Defant, F., 1951. Local winds, Compendium of Meteorology, Am. Met. Soc.; 655-672. Dixit, C. Mo and J. R. Nicholsons1964. The sea breeze at and near Bombay. Indian J. of Met. and Geophyo 15; 603-608. Eddy, G. Ao, 1966. The Texas Coast Sea Breeze: A Pilot Study. Weather, 21; 162-1700 Elder, F. Co, 1964. A facility for air-sea interaction study on Lake Michigan. Proc. 7th Conf. on Great Lakes Res., Great Lakes Res. Div., Pub. No. 11; 228-237. -81 -

Estoque, M. A o 1961. A theoretical investigation of the sea breezeo Quarto Jo Roy. Met. Soc., 87; 136-146. Estoque, M A., o 1962. The sea breeze as a function of the prevailing synoptic situation. Jo Atm. Sco 19; 244o250o Fisher, E. L., 1960. An observational study of the sea breeze. J. of Meto, 18; 645-660. Frizzola, Jo Ao and E. Lo Fisher, 1963. A series of sea breeze observations irn the New York City area. J. Appl. Met., 2; 722-739. Fujita, T., 1965. Mesometeorological Field Studies. University of Chicago, Department of Geophysical Sciences, Final Report, Contract AF 19 (604)-7259. Hall, C. D., 1954. Forecasting the lake breeze and its effects on visibility at Chigago Midway Airport. Bullo Amo Met. Soc., 35; 105-111. Hass, W. A., W. H. Hoecker, D. Ho Pack, and J. Ko Angell, 1967. Analysis of Low-Level, Constant Volume Balloon (Tetroon) Flights over New York City. Quart. J. Roy. Met.. Soc., 9 3; 483-493. Hewson, E. W, Go C Go Gill Eo W. Bierly, and I. Spickler, 1960. Meteorological analysis. Rep. No. 2515-5-P, Univ. of Mich. Res. Inst.o Ann Arbor, Mich. Hewson, E. W., Go Co Gill, and G. Jo Walke, 1963, Smoke plume photography study, Big Rock Point Nuclear Plant, Char levoix, Micho Repo No. 04015-3-P, Univ. of Mich. Res. Inst, Ann Arbor, Mich.

-83 -Hewson, E. W, and L. E. Olsson, 1967. Lake effects on air pollution dispersion. J. Air Poll. Cont-. Assoc., 17; 757-761. Lansing, L., 1965. Air mass modification by Lake Ontario during the April-November period. Proc. 8th Conf. on Great Lakes Res., Great Lakes Res. Div., Pub. No. 13; 257-261. Lyons, W. A., 1967. Photographic investigation of The lake breeze front. Film Presented at the Conf. on Physical Processes of the lower Atmosphere, Ann Arbor, Mich. Lyons, W. A., 1966. Some effects of Lake Michigan upon squall lines and summertime convection. Proc. 9th Conf. on Great Lakes Res., Great Lakes Res. Div., Pub. No. 15, 259-273. McPherson, R. D., 1968. A three-dimension numerical study of the Texas coast sea breeze. 'Rep. No. 15. Atmospheric Science Group, Coll. of Eng., Univ. of Texas, Austin, Texas; 252 pp. Moroz, W. J., 1965. The lake breeze circulation along the shoreline of a large lake. PhD Thesis, Dept. of Meteorology and Oceanography, Univ. of Mich., Ann Arbor; 120 pp. Moroz, W. J., 1967. A lake breeze on the eastern' shore of Lake Michigan: Observations and model. J. Atm. S., 24; 337-355. Munn, R. E. and T. L. Richards, 1964. The lake breeze: A survey of the literature and some applications to the Great Lakes. Proc. 7th Conf. on Great Lakes Res., Great Lakes Res. Div., No. 11; 253-266.

-84 -Olsson, L. E., A. L. Cole, and E. W. Hewson, 1968. An observational study of the lake breeze on the eastern shore of Lake Michigan, June 24-25, 1965. Proc. 11th Conf. on Great Lakes Res., Int. Assoc. Great Lakes Res., Ann Arbor, Mich., In Press. Pack, D. H. and J. K. Angell, 1963. A preliminary study of air trajectories in the Los Angeles Basin as derived from tetroon flights. Mon. Weath. Rev., 91; 583-604. Strong, A. E. and F. R. Bellaire, 1967. The overwater development of a lake breeze in an offshore gradient flow. Proc. 1;0 th Conf. on Great Lakes Res., Int. Assoc. Great Lakes Res., Ann Arbor; 240-250. Strong, A. E., 1968. The spring lake anticuclone: Its inducement on the atmospheric and water circulations. PhD Thesis, Spec. Rep. #34, Great Lakes Res. Div., Inst. of Sc. and Tech., Univ. of Michigan.; 146 pp. van Bemmelen, W., 1922. Land-und seebrise in Batavia. Beitrage zur Phys ik der freien Atmosphare, 10; 169-17/. Wallington, C. E., 1959. The Structure of the sea-breeze front as revealed by gliding flights. Weather, 14; 263-270. Wallington, C. E., 1965. Gliding through a sea breeze front. Weather, 20; 140-144. Wexler, R., 1946. Theory and observations of land and sea breezes. Bull. Am. Met. Soc., 27; 272-287.

-85 — APPENDIX TABULATION OF DATA

TABLE Al. Dry bulb temperature (T) in ~C, relative humidity (RH) in %, dew point temperature (Td) in ~C and solar radiation (SR) in cal cm-2 min-1 for several stations near an observation line south of Grand Haven, Michigan, 25 June, 1965. Subscripts u, L and w in the MYSIS column indicate upper sensor (11.8 m above surface), lower sensor (5.1 m above surface) and water temperature (1.2 m below surface) respective. MYSIS' off shore distance (X) in km is given. TIME 81 LAKE SHORE a8 KM 16 K14 24 KM MYSIS GRR TIM 2.5m 0 KM RH SR T RHT T RHT K T T T T T RH T T RH T T T RH Td d T RH Td 0030 9.0 11.7 71 6.6 0.00 11.1 76 7.0 10.6 93 9.5 0030 0100......3 12.2 70 6.9 0.00 10.0 82 7.0 10.0 96 9.4 11.1 89 9.4 12.2 83 9.4 15.0 72 10.0 0100 0130 8.0 12.2 72 7.3 0.00 9.4 87 7.3 10.0 96 9.4 0130 0200 7.8 11.7 74 7.2 0.00 9.4 87 7.3 9.4 96 8.8 10.6 88 8.7 12.2 8.9 13.9 10.0 0200 0230 7.5 12.2 73 7.5 0.00 8.9 91 7.5 9.4 95 8.6 0230 0300 8.2 12.2 75 7.9 0.00 8.3 94 7.4.8.9 96 8.3 10.0 89 8.5 10.6 9.4 12.8 10.0 0300 0330 6.9 12.2 76 8.1 0.00 7.2 96 6.6 8.3 96 7.7 0330 0400 5.6 11.7 77 7.8 0.00 6.7 96 6.1 7.8 97 7.3I 9.4 90 7.8 10.6 83 7.8 12.2 83 9.4 0400 0430 6.6 11.1 82 8.1 0.00 6.1 96 5.6 7.8 97 7.3 0430 0500 5.7 10.6 83 7.8 0.00 5.6 96 5.0 7.2 97 6.8 8.9 88 7.0 10.0 7.8 11.1 9.4 0500 0530 7.5 10.6 83 7.8 0.01 5.0 96 4.5 7.2 97 6.8 0530 0600 5.5 10.6 84 8.0 0.05 4.4 96 3.9 7.2 98 7.0 9.4 83 6.6 -1.6 11.7 11.5 6.1 13.0 9.4 7.8 11.1 9.4 0600 0630 10.4 10.6 82 7.6 0.30 5.6 96 5.0 7.8 98 7.5 -1.6 12.5 12.3 6.9 13.2 0630 0700 11.5 11.7 75 7.5 0.50 8.9 90 7.3 10.0 90 8.4 11.7 75 7.4 -6.4 13.2 13.2 7.5 14.1 11.1 86 8.9 13.3 80 10.0 0700 0730 12.5 13.3 70 8.0 0.65 11.7 76 7.6 12.8 76 8.7 -6.4 13.2 13.3 7.7 13.7 0730 0800 14.5 14.4 64 7.7 0.78 13.9 64 7.2 14.4 67 8.4 13.9 62 6.8 -6.0 14.2 14.2 8.0 14.2 15.0 10.0 16.7 10.0 0600 0830 16.1 15.6 59 7.6 0.90 15.6 57 7.1 15.6 62 8.4 -4.8 14.7 14.7 7.9 13.8 0830 0900 17.3 17.2 55 8.1 1.02 17.2 51 7.0 16.7 57 8.2 16.7 50 6.3 -1.6 15.6 15.5 7.8 12.9 17.8 10.6 18.9 9.4 0900 0930 18.4 18.3 51 8.0 1.08 18.3 47 6.1 17.8 51 7.5 -1.6 16.4 16.3 8.0 13.1 0930 0' 1000 18.5 19.4 49 8.4 1.14 19.4 43 6.5 18.9 47 7.4 18.3 43 5.5 -1.6 17.0 17.0 7.9 13.3 18.9 97 10.0 20.0 31 9.4 1000 1030 20.7 20.6 43 7.6 1.18 20.6 40 6.6 20.0 44 7.4 -6.4 16.1 16.0 9.2 14.7 1030 1100 20.8 21.7 40 7.5 1.20 21.1 37 5.8 20.6 42 7.3 19.4 38 4.7 -6.4 15.4 15.4 10.8 15.0 20.4 10.6 21.7 7.8 1100 1130 21.5 21.7 52 11.4 1.23 21.7 36 6.0 21.1 40 7.0 -1.6 15.7 15.6 10.1 13.9 1130 1200 21.4 20.6 58 12.1 1.26 22.2 34 5.6 21.7 40 7.5 20.6 36 5.0 -1.6 15.5 15.5 10.1 13.9 20.6 10.0 22.2 7.2 1200 1230 22.4 21.1 60 13.1 1.25 22.2 33 5.2 22.2 38 7.2 -1.6 14.9 15.0 10.3 14.0 1230 1300 22.6 20.0 64 13.0 1.24 22.2 33 5.2 22.2 38 7.2 21.7 36 6.0 -1.6 14.6 14.7 9.6 14.5 21.7 48 10.0 23.3 34 7.2 1300 1330 22.4 20.0 62 12.5 1.22 22.8 33 5.7 22.8 38 7.8 -6.4 15.0 15.0 9.3 15.2 1330 1400 22.8 20.0 62 12.5 1.21 23.3 31 5.2 23.3 38 8.2 22.2 40 8.0 -6.4 14.5 14.6 9.4 15.3 21.7 8.9 22.2 10.6 1400 1430 23.2 18.9 66 12.5 1.15 23.3 31 5.2 23.3 38 8.2 -1.5 14.8 14.6 9.4 14.9 1430 1500 23.0 18.9 67 12.7 1.10 23.9 31 5.8 23.3 36 7.4 22.8 40 8.5 23.7 10.0 22.2 10.6 1500 1530 23.7 18.3 68 12.3 1.00 23.9 31 5.8 23.9 36 7.9 1530 1600 22.1 17.8 68 11,8 0.90 23.9 36 8.0 23.9 36 7.9 23.3 40 9.0 22.8 40 8.3 22.8 44 10.0 1600 1630 22.3 17.8 67 11.6 0.80 22.2 39 7.6 24.4 36 8.4 1630 1700 21.4 17.8 67 11.6 0.70 21.7 40 7.5 24.4 35 8.0 23.3 40 9.0 23.3 7.8 22.2 9.4 1700 1730 21.4 17.8 68 11.8 0.54 21.1 41 7.3 24.4 36.8.4 1730 1800 20.3 17.2 68 11.3 0.42 20.6 42 7.3 24.4 36 8.4 22.8 36 6.9 22.8 8.3 22.2 9.4 1800 1830 20.5 16.7 68 10.6 0.29 20.6 42 7.3 23.3 41 9.3 1830 1900 20.0 16.7 67 10.5 0.16 20.0 43 7.0 22.2 43 9.0 22.2 39 7.6 22.8 38 7.8 22.2 44 10.0 1900 1930 19.6 17.2 58 8.9 0.05 20.0 45 7.7 21.7 47 9.9 -1.8 15.6 15.4 9.4 14.4 1930 2000 19.0 17.2 60 9.4 0.02 19.4 48 8.1 21.1 52 10.9 21.7 46 9.6 -1.8 16.0 15.5 9.8 14.4 21.1 9.4 21.1 10.6 2000 2030 16.8 16.7 63 9'6 0.00 17.8 60 9.9 18.9 66 12.4 -1.8 17.3 16.0 9.2 14.3 2030 2100 13.9 16.1 67 10.0 0.00 15.6 77 11.6 17.2 80 13.7 17.8 64 10.9 -1.8 17.0 16.4 9.1 14.4 18.3 10.6 19.4 10.0 2100 2130 13.6 15.6 72 10.6 0.00 13.9 84 11.2 15.6 88 13.6 -0.5 18.6 17.8 9.5 15.5 2130 2200 14.2 15.0 77 11.0 0.00 12.8 90 11.2 14.4 92 13.1 16.1 78 12.3 16.7 67 10.6 17.8 63 10.6 2200 2230 12.3 14.4 78 10.6 0.00 11.7 91 10.3 13.3 94 12.4 2230 2300 13.0 14.4 80 11.0 0.00 10.6 92 9.4 13.3 94 12.4 15.0 84 12.3 2300 2330 13.4 14.4 76 10.3 0.00 11.1 90 9.5 13.9 85 11.4 2330 2400 14.2 15.0 71 9.8 0.00 12.2 80 8.9 14.4 69 8.8 15.0 86 12.7 2400

TABLE A2. Air and soil temperatures in 0C at various heights respective depth at the WJBL station north of Holland1Michigan,, 25 June,, 1965. Height Above Ground in H TIME -1.00 -0.10 -0.01 2.4 4.9 9.8 19.5 39.0 78.0 0030 15.5 15.0 20.1 9. 0 9.9 11.5 12. 7 13.9 14.4 0100 15.3 19.4 15.5 8.3 9.8 10.9 12.2 13.5 15.1 0130 15.5 19.2 15.4 8.0 8.6 11.0 12.2 13.6 14.9 0200 15.2 18.7 14.6 7.8 8.5 10.1 12.0 13.1 14.2 0230 15.4 18.6 14.5 7.5 8.5 10.2 11.5 13.2 13.9 0300 15.1 17.9 13.9 8.2 8.5 9.0 10.1 11.6 12.8 0330 15.4 18.0 13.8 6.9 7.5 8.9 10.6 11.9 13.1 0400 15.2 17.4 13.3 5.6 6.7 8.5 10.6 12.5 12.6 0430 15.4 17.3 13.0 6.6 6.9 7.5 10.6 12.1 13.1 0500 15.2 16.6 12.5 5.7 6.8 8.5 9.9 11.8 12.2 0530.15.5 16.6 12.4 7.5 8.0 9.0 9.5 11.0 12.0 0600 15.1 16.0 12.0 5.5 6.5 8.0 9.9 10.9 11.2 0630 15.5 16.1 12.1 10.4 10.0 10.3 10.6 11.4 12.3 0700 15.2 15.5 13.0 11.5 11.5 11.5 11.2 11.0 11.9 0730 15.4 15`5 13.6 12.5 12.8 12.8 12.4 12.3 12.0 0800 15.4 15.5 15.0 14.6 14.7 14.4 13.8 13.5 13.4 0830 15.9 15.9 17.5 1E~.i 15.9 15.6 15.4 15.0 14.5 0900 15.5 15.9 19.4 17.3 17.4 16.5 16.0 16.0 15.4 0930 16.0 16.5 22.5 18.4 18.0 17.5 17.4 16.7 16.4 1000 15.5 17.0 25.0 18.5 18.2 17.6 17.5 17.4 16.6 1030 16.0 17.6 27.6 20.7 19.8 19.7 19.0 18.5 17.9 1100 15.5 18.0 29.8 20.8 19.9 19.0 18.2 18.0 17.6 1130 16.1 19.0 31.6 21.5 21.1 21.3 20.2 19.2 19.0 1200 15.6 19.5 32.8 21.4 20.7 20.3 19. 7.19.4 19.0 1230 16.3 20.7 34.0 22.4 21.3 21.1 21.1 20.3 20.0 1300 15.6 21.3 34.4 22.6 21.9 21.8 21.2 20.4 19.6 1330 16.2 22.4 35.7 22.4 22.0 21.6 21.6 20.7 20.6 1400 15.6 23.0 37.0 22.8 22.1 21.9 21.4 20.7 20.4 1430 16.3 23.9 37.9 23.2 22.9 22.5 22.1 21.5 21.0 1500 15.7 24.3 38.0 23.0 22.6 22.3 21.8 21.3 21.1 1530 16.3 25.2 37.5 23.7 23.0 22.7 2~.O 21.7 21.0 1600 15.7 25.3 36.0 22.1 21.8 21.4 20..9 20.9 20.3 1630 16.3 26.0 35.2 22.3 21.9 21.3 20%.5 20.1 20.0 1700 15.7 25.8 33.3 21.4 21.3 20.6 20.1 19.8 19.3 1730 16.2 26.2 31.7 21.4 21.3 20.3 20.0 19.4 19.0 1800 15.7 25.7 29.9 20-3 19.8 19.5 19.1 18.9 18.5 1830 16.3 26.0 28.3 20.5 20.3 20.0 19.5 19.1 18.7 1900 15.5 25.2 26.4 20.0 19.7 19.6 19.3 19.2 18.5 1930 16.1 25.2 25.1 19.6 19.5 19.5 19.4 19.1 18.5 2000 15.5 24.5 23.8 -19.0 18.5 18.7 18.9 18.6 18.7 2030 16.0 24.4 22.6 16.8 17.0 17.4 17.6 17.9 19.9 2100 15.4 23.6 21.0 13.9 14.6 15.5 16.7 18.8 19.9 2130 15.9 23.5 20.1 13.6 14.8 15.4 16.8 19.e- 20.1 2200 15.4 22.7 19.1 14.2 14.3 15.0 17.0 19.5 20.0 2230 15.7 22.4 18.8 12.3 13.0 15.5 16.6 18.7 20.3 2300 15.3 21.7 17.9 13.0 13.5 14.6 15.4 17.6 19.0) 2330 15.7 21.5 17.6 13.4 13.8 14.9 15.6 17.3 18.5 2400 15.3 20.7 17.3 14.2 14.3 14.4 15.2 16.2 17.5

TABLE A3. Air temperature (T) in 0C, wet bulb temperature (Tv) in OC, relative humidity (RH) in %, and water vapor pressure (e) 'in rab, observed from aircrafts in a cross section along an ob&. serva~tion line south of Grand Haven, Michigan, 25 June, 1965. Time is EST. Position coordinates for the aircraft are given -in meters0 X-direction is perpendicular to the shore and X is positive toward the east and zero at the shore. Z. is positive upward.

Time Aircraft position Temperature and Moisture X Z T TW e RH 073710 32188.0 152.5 13.4 10.3 8.687 68.0 074000 7242.3 152.5 12.9 10.0 8.303 65.0 074500 8690.7 152.5 13.0 10.2 9.070 71.0 074750.0 152.5 13.2 10.2 8.814 69.0 074900 -2575.0 152.5 13.7 10.1 8.176 64.0 075000 - 5311.0 152.5 13.4 10.2 8.431 66.0 075100 -8047.0 152.5 13.7 10.1 8.176 64.0 075500 - 18669.0 152.5 14.6 10.4 7.665 60.0 080000 -32188.0 152.5 14.7 9.8 6.381 52.0 080030 -32188.0 305.0 14.3 9.1 6.011 51.0 080205 -32188.0 457.5 14.2 8.4 5.014 44.0 080335 -32188.0 610.0 13.7 7.0 3.552 35.0 080505 -321.88.0 762.5 12.4 6.1 3.531 36.0 080655 -32188.0 915.0 10.9 5.5 3.952 42.0 080840 -32188.0 1067.5 9.6 5.0 4.363 48.0 081025 -32188.0 12200.0 8.4 4.5 4.708 54.0 081225 -32188.0 1372.5 7.3 3.1 4.101 53.0 081425 -321-88.0 1525.0 6.7 1.8 2.719 38.0 081625 -32188.0 1677.5 6.2 -.1 1.221 20.0 081855 -32188.0 1830.0 6.2 -.1 1.221 20.0 082115 -32188.0 1982.5 5.6 082330 - 32188.0 2135.0 5.6 083000 - 17703.4 2135.0 6.2 083500 - 6598.5 2135.0 6.2 083800.0 2135.0 6.2 084500 20278.4 2135.0 6.7 084930 32188.0O 21-35.0 6.6 085055 32188.0 1982.5 6.9 085215 32188.0 1830.0 7.2 -.6.292 5.0 085345 32188.0 1677.5 7.5.2 1.020 16.0 085510 32188.0 1525.0, 7.9.1.701 11.0 085650 32188.0 1-372.5 8.6.6.727 11.0 08581.0 321-88.0 1220.0 9.0 1.8 1.502 21.0 085940 32188.0 1067.5 9.0 3.1 2.553 33.0 090100 32.188.0 915.0 10.0 4.4 3.313 38.0 090220 32188.0 762.5 10.6 6.2 5.002 51.0 090350 32188.0 610.0 11.2 8.5 7.749 68.0 090515 32188.0 457.5 12.9 9.5 7.976 65.0 090635 32188.0 305.0 14.1 10.3 8.048 63.0 090745 32188.0 152.5 15.6 11.1 7.283 53.0

Time Aircraft position Temperature and Moisture X Z T T ~ e RH 095300 32188.0 152.5 16.5 11.2 7.145 52.0 1-00000 11587.6 152.5 16.5 11.3 7.283 53.0 100405.0 152.5 17.0 11.2 6.596 48.0 101000.-16737.7 152.5 15.1 11.0 8.056 61.0 101530 -32188.O 152.5 14.6 10.6 8.188 62.0 101630 -32188.0 305.0 14.2 9.3 6.129 52.0 101750 -32188.0 457.5 13.4 7.8 4.924 45.0 101905 -32188.0 610.0 1-3.5 5.7 2.446 26.0 102025 -32188.0 762.5 12.1 5.3 2.909 32.0 102155 -32188.0 915.0 11.0O 3.9 2.257 27.0 102320 -32188.0 1067.5 10.4 4.3 2.842 34.0 102500-32188.0 1220.0 9.0 4.3 3.84.6 46.0O 102625 -32188.0 1372'.5 8.0 2.8 3.017 39.0 102805 -32188.0 1525.0 8.4.2.510 8.0 103030 -32188.0 1677.5 8.0.1.637 10.0 103220 -32188.0 1830.0 7.6 -.4.366 6.0 103425 -32188.0 1982.5 6.6 103640 -32188.0 2135.0 5.9 104000 -25267.5 2135.0 6.5 104200 -2:O0600.3 2135.0 6.2 104500...13840.8 2135.0 6.3 105000 - 2253.1 2135.0 6.6 105100.0O 2135.0 6.5 105500 10300.1 2135.0 6.5 110000 23336.3 2135.0 6.5 110320 32188.0 2135.0 6.7 110455 32188.0 1982.5 6.9 110605 32188.0 1830.0 7.6 -.8.058 1.0 L10730 32188.0 1677.5 8.3.1.701 11.0 110905 32188.0 1525.0 8.4 -.2.061 1.0 111040 32188.0 1372.5 9.5.4.127 2.0 '111210 32188.0 1220.0 9.1 2.0 1.431 20.0.111340 32188.0 1067.5 8.7 5.8 6.023 64.0 111500 32188.0 915.0 10.3 7.0 6.192 61.0 111610 32188.0 762.5 11.6 8.1l 6.784 62.0 111720 32188.0 610.0 13.0 876.382 56.0 111840 32188.0 457.5 14.7 9.6 6.872 56.0 L12000 32188.0 305.0 15.9 10.3 6.259 49.0 11210532188.0.0 152.45 17.5 10.8 ia5.546 42.0

Time Aircraft position Temperature and Moisture X Z T TW e RH 123145 32188.0 152.5 18.-9 12.2 6.352 43.0 123500 21405.0 152.5 19.0 11.7 5.681 40.0 124000 9334.5 152.5 19.1 11.8 5.681 40.0 124330.0 152.5 17.3 11.0 5.943 45.0 124500 - 3701. -6 152.5.17.3 11.2 6.321 46.0 125000 -16094.0 152.5 16.9 10.9 6.075 46.0 125615 -32188.0 152.5 16.4 8.7 3.647 32.0 125650 -32188.0 305.0 15.5 8.1 3.611 33.0 125805 -32188.0 457.5 14.4 7.2 3.384 32.0 125945 -32188.0 610.0 13.4 5.9 2.541 27.0 130100 -32188.0 762.5 12.1 5.1 2.636 29.0 130235 -32188.0 915.0 10-.6 3.6 2.098 26.0 130405 -32188.0 1067.5 10.2 2.3.1.344 18.0 130550 -32188.0 1220.0 9.7 1.5.828 12.0 130735 -32-188.0 1372.5 9-.3. 3.191 3.0 130920 -32188.0 1525.0 9.0 -. 1 131100 -32188.0 1677.5 8.0.2..574 9.0 131245 -32188.0 1830.0 8.0 -.4.122 2.0 131435 -32188.0 1982.5 7.1 -1.0.116 2.0 131645 -32188.0 2135.0 6.5 132000 -25750.4 2135.0 6.9 132500 -14967.4 2135.0 6.6 133200.0 2135.0 6.5 133500 7403.2 2135.0 7.0 134445 32188.0 2135.0 6.5 134630 32188.0 1982.5 6.5 134745 32188.0 1830.0 6.5.6.643 11,0 134905 32188.0 1677.5 6.8 1.7 2.647 37.0 135030 32188.0 1525.0 6.7 3.7 4.924 61.0 1-35145 32188.0 1372.5 7,6 5.9 7.435 79.0 135 250 32188.0 1220'0 9.2 6.9 7.207 71.0 135400 32188.0 1067.5 10.7 7.6 6.875 65.0 135545 32188.0 915.0 12.2 8.7 7.180 63.0 135730 32188.0 762.5 13.6 6.,7 3'.349 33.0 135840 32188.0 610.0 15.1 10.2 6.898 54.0 140030 32188.0 457.5 16.5 10.8 6.603 50.0 140245 32188.0 305.0 18.5 11.9 6.533 46.0 140400 32188.0 152.5 20.1 12.7 6.106 40.0

TABLE A4. Wind direction (WD) in degrees and wind speeds in m sec-1 for several stations near an observation line south of Grand Haven, Michigan, 25 June, 1965. VT indicates total horizontal vector wind, U the across shore component - onshore wind is positive and from the west -, and V the along shore component - southerly wind is positive. Winds at three levels at WJBL are given. MYSIS' off shore distance (X) in km is given. TIME WJBL LAKE 8 KM 16 KM LAKE TIME SHORE TOWER 10 M 20 M 40 M WD VT U V WD VT U V WD VT U V WD VT WD VT U V WD VT U V WD VT U V X WD VT U V WD VT U V WD VT U V 0030 45 1.0 045 1.5 -1.1 -1.1 0 0 0 0 360 2.1 0 -2.1 0030 0100 0 0 0 0 045 1.8 -1.3 -1.3 055 4.0 -3.3 -2.3 045 0.7 -0.5 -0.5 0 0: 050 4.1 -3.2 -2.6 010 2.1 -0.4 -2.1 030 2.6 -1.3 -2.3 0100 0130 360 0.5 0 -0.5 270 0.9 0.9 0 040 3.1 -2.0 -2.4 0130 0200 0 0 0 0 050 1.8 -1.4 -1.2 075 4.0 -3.9 -1.0 360 0.6 0 -0.6 270 1.0 1.0 0 060 3.1 -2.7 -1.6 0 0 0 0 040 2.1 -1.4 -1.6 0200 0230 360 0.5 0 -0.5 270 0.9 0.9 0 060 1.5 -1.3 -0.8 0230 0300 0 0 0 0 055 1.8 -1.5 -1.0 075 3.6 -3.5 -0.9 0 0 0 0 0 0 0 0 060 2.1 -1.8 -1.1 340 1.5 0.5 -1.4 030 2.6 -1.3 -2.3 0300 0330 360 0.5 0 -0.5 315 0.5 0.4 -0.4 050 3.6 -2.8 -2.3 0330 0400 0 0 0 0 085 1.8 -1.8 -0.2 095 2.2 -2.2 0.2 45 4.0 0 0 0 0 0 0 0 0 050 3.6 -2.8 -2.3 060 2.6 -2.3 -1.3 040 2.1 -1.4 -1.6 0400 0430 0 0 0 0 0 0 0 0 060 3.6 -3.1 -1.8 0430 0500 0 0 0 0 075 1.8 -1.7 -0.5 085 3.6 -3.6 -0.3 0 0 0 0 0 0 0 0 060 3.6 -3.1 -1.8 030 2.6 -1.3 -2.3 050 2.1 -1.6 -1.4 0500 0530 360 0.9 0 -0.9 0 0 0 0 060 4.6 -4.0 -2.3 0520 0600 085 1.3 -1.3 -0.1 095 1.8 -1.8 0.2 095 3.6 —3.6 0.3 0 0 0 0 0 0 0 0 070 4.1 -3.9 -1.4 -1.6 110 4.6 -4.3 1.6 060 2.6 -2.3 -1.3 060 2.1 -1.8 -1.1 0600 0630 0 0 0 0 0 0 0 0 070 4.6 -4.3 -1.6 -1.6 125 5.1 -4.2 2.9 0630 0700 115 1.3 -1.2 0.6 120 2.2 -1.9 1.1 115 3.1 -2.8 1.3 045 1.5 -1.1 -1.1 360 0.3 0 -0.3 080 4.6 -4.4 -0.8 -6.4 105 2.6 -2.5 0.7 060 2.6 -2.3 -1.3 110 3.1 -2.9 1.1 0700 0730 045 2.7 -1.9 -1.9 015 1.8 -0.4 -1.7 080 4.6 -4.4 -0.8 0730 0800 110 2.2 -2.1 0.8 130 2.7 -2.0 1.7 125 2.7 -1.9 1.9 90 2.5 090 3.3 -3.3 0 045 2.4 -1.7 -1.7 070 4.1 -4.0 -2.3 050 4.1 -3.1 -2.6 110 3.6 -3.4 1.2 0800 0830 135 3.6 -2.6 2.6 045 2.4 -1.7 -1.7 080 4.6 -4.4 -0.8 4.8 110 3.1 -2.9 1.1 0830 0900 110 3.1 -2.9 1.1 120 3.6 -3.1 1.8 115 3.1 -2.8 1.3 090 3.3 -3.3 0 080 1.9 -1.9 -0.3 090 4.6 -4.6 0 -1.6 085 2.6 -2.6 -0.2 080 5.2 -5.1 -0.9 100 3.6 -3.5 0.6 0900 0930 110 3.3 -3.1 1.1 060 2.2 -1.9 -1.1 100 2.6 -2.6 0.5 -1.6 085 2.6 -2.6 -0.2 0930 1000 095 2.7 -2.7 0.2 105 2.7 -2.6 0.7 110 2.7 -2.5 0.9 090 3.0 -3.0 0 045 1.8 -1.3 -1.3 110 2.1 -2.0 0.7 070 4.1 -3.1 -1.4 090 3.1 -3.1 0 1000 1030 080 2.5 -2.5 -0.4 045 1.6 -1.1 -1.1 240 2.1 1.8 1.1 -6.4 000 0 0 0 1030 1100 085 2.2 -2.2 -0.2 090 2.7 -2.7 0 090 2.7 -2.7 0 090 2.2 -2.2 0 360 1.6 0. -1.6 250 2.1 2.0 0.7 -6.4 290 2.1 2.0 -0.7 060 2.6 -2.2 -1.3 050 2.6 -2.0 -1.7 1100 1130 090 2.4 -2.4 0 010 1.8 -0.3 -1.8 290 2.6 2.4 -0.9 -1.6 270 4.1 4.1 0 1130 1200 055 1.8 -1.5 -1.0 080 2.2 -2.2 -0.4 080 1.8 -1.8 -0.3 360 2.5 110 1.9 -1.8 0.7 360 1.9 0 -1.9 280 2.6 2.6 -0.5 ~1.3 275 4.6 4.6 -0.4 030 4.6 -2.3 -4.0 090 2.6 -2.6 0 1200 1230 090 2.1 -2.1 0 360 1.9 0 -1.9 320 2.1 1.4 -1.6 1230 1300 M 2.2 - - 060 2.7 -2.3 -1.3 075 2.2 -2.2 -0.6 090 2.5 -2.5 0 045 1.8 -1.3 -1.3 310 3.1 2.4 -2.0 -1.6 305 4.6 3.8 -2.6 300 2.6 2.3 -1.3 170 2.1 0 2.1 1300 1330 090 2.8 -2.8 0 045 2.1 -1.5 -1.5 310 3.6 2.8 -2.3 1330 1400 060 1.8 -1.6 -0.9 080 2.7 -2.6 -0.5 075 2.2 -2.2 -0.6 110 2.5 -2.4 0.9 020 2.2 -0.8 -2.1 320 3.6 2.3 -2.8 -6.4 350 3.6 0.6 -3.6 080 4.1 -4.0 -0.7 300 4.1 3.6 -2.1 1400 1430 110 2.1 -2.0 0.7 045 1.9 -1.3 -1.3 330 4.6 2.3 -4.0 1430 1500 080 2.7 -2.6 -0.5 095 2.2 -2.2 0.2 090 2.2 -2.2 0 105 2.4 -2.3 0.6 025 1.8 -0.8 -1.6 330 4.1 2.1 -3.6 090 2.6 -2.6 0 310 3.1 2.4 -2.0 1500 1530 110 2.5 -2.4 0.9 065 1.8 -1.6 -0.8 330 4.6 2.3 -4.0 1530 1600 M 2.7 - - 110 2.7 -2.5 0.9 105 2.7 -2.6 0.7 315 2.5 290 2.5 2.4 -0.9 055 2.2 -1.8 -1.3 330 5.2 2.6 -4.5 120 4.6 -4.0 2.3 330 3.1 1.6 -2.7 1600 1630 290 4.8 4.5 -1.6 090 1.6 -1.6 0 330 4.6 2.3 -4.0 1630 1700 300 4.0 3.5 -2.0 320 4.0 2.6 -3.1 325 3.6 2.0 -2.9 290 4.0 3.8 -1.4 100 1.5 -1.5 0.3 330 5.7 2.9 -4.9 110 3.6 -3.4 1.2 310 3.1 2.4 -2.0 1700 1730 305 4.6 3.8 -2.6 090 1.9 -1.9 0 330 5.7 2.9 -4.9 1730 1800 315 4.0 2.8 -2.8 330 3.6 1.8 -3.1 325 3.1 1.8 -2.6 290 4.2 4.0 -1.4 090 1.8 -1.8 0 330 5.2 2.6 -4.5 120 2.1 -1.8 1.1 300 2.6 2.3 -1.3 1800 1830 285 3.0 2.8:-0.8 250 2.1 2.0 0.7 340 5.2 1.8 -4.9 1830 1900 330 2.7 1.3 -2.3 360 2.7 0 -2.7 335 2.7 1.1 -2.4 280 2.4 2.4 -0.4 250 1.6 1.5 0.5 340 4.1 1.4 -3.9 090 3.1 -3.1 0 300 2.6 2.3 -1.3 1900 1930 270 1.2 1.2 0 260 1.0 1.0 0.2 350 3.6 0.6 -3.6 -1.8 040 4.4 -2.8 -3.4 1930 2000 360 2.2 0 -2.2 360 2.7 0 -2.7 010 3.1 -0.5 -3.1 90 1.0 0 0 0 0 270 0.6 0.6 0 010 2.6 -0.5 -2.6 -1.8 025 2.3 -1.0 -2.1 070 2.1 -2.0 -0.7 020 3.1 -1.1 -2.9 2000 2030 0 0 0 0 0 0 0 0 030 1.5 -0.8 -1.3 1.8 064 1.4 -1.3 -0.6 2030 2100 030 1.8 -0.8 -1.6 040 3.1 -2.0 -2.4 055 3.6 -2.9 -2.0 0 0 0 0 0 0 0 0 040 2.1 -1.4 -1.6 060 2.1 -1.8 -1.1 030 2.6 -1.3 -2.3 2100 2130 0 0 0 0 0 0 0 0 060 2.6 -2.3 -1.3 2130 2200 055 1.3 -1.1 -0.8 075 3.1 -3.0 -0.8 090 2.7 -2.7 0 360 0.7 0 -0.7 0 0 0 0 070 3.6 -3.4 -1.2 090 2.6 -2.6 0 100 2.6 -2.6 0.5 2200 2230 045 1.5 -1.1 -1.1 0 0 0 0 080 3.6 -3.5 -0.6 2230 2300 090 1.8 -1.8 0 110 3.6 -3.4 1.2 120 4.9 -4.3 2.5 045 2.1 -1.5 -1.5 045 0.9 -0.6 -0.6 090 4.1 -4.1 0 2300 2330 045 3.3 -2.3 -2.3 065 1.3 -1.2 -0.6 090 5.2 -5.2 0 2330 2400 110 2.7 -2.5 0.9 120 3.6 -3.1 1.8 125 6.3 -5.1 3.6 90 4.0 045 2.5 -1.8 -1.8 090 2.1 -2.1 0 100 5.7 -5.6 1.0 2400

-93 -TABLE A5. Analyses of-pi'bal observations made at stations along an observation line south of Grand Haven, Michigan, 25 June, 1965. Time 'is ESTO Position coordinates.for the balloon are given in meters. X-" direction is pepnicular to the shore and x is positive inland toward the east and zero at the shore. Y-direction is parallel to the shore and V is positive toward north. Z is positive upward. Wind speeds are given in m sec1 VT is horizontal vector wind, and U, V, and W components are positive along positive X, Y, and Z a-xes r(espec~ —velyThe data presented in this tabulation are summarized in Table 1 on page 19. Analyses of tracks made on balloons released from the MYSIS are presented first, followed by the double theodolite analyses made on balloons released from the Lake shore station, and the single theodolite analyses made on.balloons released from that station0 Double theodolite analyses preceed single theodolite analyses also for the releases from the 8 km station.

Single Theodolite Data - Shoreline,Station - MYSIS Time Balloon Position Wind Velocit X Y Z U V VT 0630.00.0.0.0 0630.50 -1866.7 -104.3 91.4 -62.22 -3.47 62.32 0631.00 -2086.1 -131.2 182.8 - 7.31 -.J9 7.37 0631.50 -2257.1 -209.3 274.3 - 5.69 -2.60 6.26 0632.00 -2368.6 -320.2 365.7 - 3.71 -3.69 5.24 0632.50 -2454.4 -436.8 457.2 - 2.79 -3.88 4.78 0633.00 -2477.4 -549.2 548.6 -.83 -3.74 3.83 0633.50 -2500.6 -660.6 640.0 -.77 -3.71 3.o79 0634.00 -2541.0 -772.0 731.5 - 1.34 -3.71 3.94 0634.50 -2578.8 -882.8 822.9 - 1.25 -3.69 3.90 0635.00 -2592.9 -1005.7 914.4 -.47 -4.09 4.12 0635.50 -2608.7 -1123.4 1005.8 -.52 -3.92 3.96 0636.00 -2643.6 -1238.3 1097.2 - 1o16 -3.82 4.00 0636.50 -2693~6 -1360.6 1188.7 - 1.66 -4.07 4.40 0637.00 -2740S;9 -1525.5 1280.1 - 1.57 -5.49 5 72 0637.50 -2767.1 -1729.0 1371.6 -.87 -6.78 6.83 0638.00 -2759.2 -1953.6 1463.0.26 -7.48 7.49 0638.50 -2756.7 -2169.2 1554.4.08 -7.18 7.18 0639.00 -2767.7 -2372.2 1645.9 -.36 -6.76 '.77 0639.50 -2806.7 -2553.8 1737.3 - 1.29 -6.05 6.19 0640.00 -2785.8 -2785.8 1828.8.69 -7.73 7.76 0640.50 -2688.7 -2923.8 1920.2 3.23 -4.60 5.62 0641.00 -2681.1 -3062.5 2011.6.25 -4.62 4.62 0641.50 -2676.2 -3189.3 2103.1.16 -4.22 4.23 0642.00 -2635.5 -3313.3 2194.5 1.35 -4.13 4.34 0642.50 -2539.4 -3491.7 2286.0 3.20 -5.94 6.75 0643.00 -2339.7 -3701.1 2377.4 6.65 -6.97 9.64

Single Theodolite Data - Shoreline Station = MYSIS Time Balloon Position Wind Velocit:y X Y Z U V VT 0900.00.0.0.0 0900.50 =1652.6 80.6 91.4 ~-55.08 2.68 55.15 0901.00 =1438.6 161.3 182.8 7.13 2.68 7.62 0901.50 =1682.4 194.6 274.3 8.12 1.11 8.20 0902.00 =1800.4 221.0 365.7 -3.93.87 4.02 0902.50 -1935.9 227.4 457.2 -4.51.21 4.52 0903.00 -2080.5 211.3 548.6 -4.82 -.53 4.85 0903.50 =2227.0 151.8 640.0 -4.88 -1.98 5.26 0904.00 =22.91.4 56.0 731.5 -2.14 -3.19 3.84 0904.50 =2363.1 =-16.4 822.9 -2.38 =2.41 3.39 0905.00 =2418.2 -88.6 914.4 -1.83 -2.40 3.02 0905.50 -2470.7 =177.0 1005.8 -1.74 =2.94 3.42 0906.00 -2490.0 -327.7 1097.2 -.64 -5.02 5.06 0906.50 =2485.8 =510.2.1188.7.14 -6.08 6.08 0907.00 =2443.0 -714.3 1280.1.1.42 -6.80 6.95 0907.50 =2412.7 -849.6 1371.6 1.00 -4.50 4.62 0908.00 =2364.1 -1047.6 1463.0 1.62 =6.59 6.79 0908.50 =2357.5 -1185.7 1554.4.21 =4.60 4.60 0909.00 -2388.6 =1318.5 1645.9 -1.03 =4.42- 4.54 0909.50 =2460.2 -1408.9 1737.3 =2.38 =3.01 3.84 0910.00 =2519.1 -1489.7 1828.8 =1.96 =2.69 3.33 0910.50 -2584.3 -1596.1 1920.2 -2.17 =3.54 4.15 0911.00 =2616.9 =1745.2 2011.6 -1.08 -4.97 5.08 0911.50 =2626.6 -1894.3 2.103.1 -.32 =4.96 4.98.0912.00 =2638.2 =2091.0 2194.5 -.38 -6.55 6.56 0912.50 -2705.8 =2230.5 2286.0 -2.25 -4.64 5.16 0913.00 =2674.3 =2459.1 2377.4 1.05 =7.62 7.69 0913.50 =2692.9 =2683.5 2468.8 -.62 =7.47 7.50 0914.00 =2684.0 =2929.0 2560.3.29 -8.18 8.19 0914.50 =2674.7 -3210.2 2651.7 031 =9.37 9.37 0915.00 =2609.4 =3488.0 2743.2 2.17 -9.26 9.51 0915.50 =2559.7 =3766.5 2834.6 1.65 =9.28 9.42 0916.00 =2482.5 -4035.2 2926.0 2.57 -8.95 9.31 0916.50 =2426.8 =4306.8 3017.5 1.85 -9.05 9.24 0917.00 =2381.1 =4593.6 3108.9 1.52 =9.56 9.68 0917.50 =2373.2 -4887.4 3200.4.26 =9.79 9.79 0918.00 =2355.4 -5192.3 3291.8. 59 -10-16 10.18 0918.50 =2279.4 =5476.0 3383.2 2.53 -9.45 9.78 0919.00 =2209.9 -5757.0 3474.7 2.31 =9.36 9.64 0919.50 =2121.4 =6059.7 3566.1 2.95 =10.09 10.51 0920.00 =2022.8 --- - - -- =6381 67. 32 =92 9.84 -

Single Theodolite Data - MYSIS Balloon Position Wind Velocit Time- X Y Z U V VT 0902.00.0.0.0 0902.50 -1706.0 - 25.8 90.0 -3.70 -0.65 3.71 0903.00 -1808.0 - 51.2 180.0O -2.60 -0.45 3.80 0903.50 -1928.2 - 69.4 270.0 -3.95 0.20 3.95 0904.00 -2044.2 - 46.5 360.0 -3.83 0.99 3.95 0904.50 -2157.7 - 9.8 450,.0 -4.31 -1.71 4.64 0905.00 -2303.0 - 149.1 540.0 -3.72 -3.32 4.99 0905.50 -2380.9 - 208.8 630.0 -1.,67 -2.64 3.13 0906.00 -2403.1 - 307.6 720.0 -1.09 -3.09 3.27 0906.50 -2446.6 - 393.,9 810.0 -2.02 -2.71 3.38 0907. 00 -2524.5 - 470.2 900.0 -.25 -2.74 2.75 0907.50 -2461.,8 - 558.5 990.0.89 -3.90 4.00 0908. 00 -2471.2 - 704.0 1080.0.,30 -5.22 5.23 0908.50 -2443.7 - 871.7 1170.0O 3.61 -7.10 7.97 0909. 00 -2254.4 -1130.1 1260.0O 4.55 -6.76 8.15 0909.50 -2170.6 - 127 7.3 1350.0 3.3 5 -5.78 6.68 0910. 00 -2053.5 -1476.9 1440.0 2.40 -5.13 5.66 0910.50 -2026.7 -1585.0 1530.0.46 -3.22 3.25 0911.00 -2080.9 -1670.1 1620.0 -1.35 -2.97 3.26 0911. 50 -2107.5 -1762.9 1710.0O -.,08 -4.50 4.50 0912.00 -2085.6 -1939.9 1800.0.89 -6.07 6.13 0912. 50 -2054.1 -2126.9 1890-0 -.12 - 6.14 6.14 0913.00 -2092.6 -2308.4 1980.0.39 -5.05 5.06 0913.50 -2030.4 -2429.,7 2070.0:.73 -3.78 3.85 0914.00 -2049.0 -2535.4 2160.0 -1,70 -4.97 5.25 0914,50 -2132.2 -2727.8 2250.0 -1.22 -6.91 7.02

S~ingle Theodolite Data - MYSIS Balloon Position Wind Velocit Time X Y Z U V VT 11OLOO0.0.0.0 1101.50 -6396.8 - 11.2 90.0.04 -1.09 1.09 1102.00 -6405.7. - 65.5 180.0 -.11 -1.91 1.91 1102.50 -6403.6 - 125.9 270.0 -.48 -1.67 1.74 1103.00 -6434.3 - 165.8 360.0 -1.65 -1.29 2.10 1103.50 -6502.8 - 203.4 450.0 -2.54 -1.49. 2.95 1104.00 -6586.8 - 255.4 540.0 -3.43 -1.62 3.79 1104.50 -6708.6 - 300.6 630.0 -3.82 -1.45 4.09 1105.00 -6816.2 - 342.6 720.0 -4.05 -1.45 4.31 1105.50 -6951.6 - 387.8 810.0 -4.33 -1.52 4.59 1106.00 -7075.8 - 433.8 900.0 -3.76 -1.55 4.07 1106.050 -7177.4 - 480.8 990.0 -3.18 -1.54 3.54 1107.00 -7266.8 - 526.3 1080.0 -2.79 -2.51 3.76 1107.50 -7344.8 - 631.9 1170.0 -1.88 -3.43 3.92 1108.00 -7379.8 - 732.4 1260.0 -.74 -3.19 3.28 1108.50 -7389.4 - 823.6 1350.0 -.44 -2.77 2.81 1109.00 -7406.0 - 898.7 1440.0 -.46 -3.09 3.12 1109.50 -7416.9 -1009.0 1530.0 -1.17 -3.46 3.65 1110.00 -7476.0 -1106.1 1620.0 -1.11 -3.44 3.62 1110.50 -7483.3 -1215.6 1710.0 -1.25 -2.73 3.00 1111.00 -7551.0 -1269.6 1800.0 -1.58 -1.03 1.88 1111.50 -7578.1 -1277.1 1890.0 -1.23 -.15 1.24 1112.00 -7624.0 -1260.3 1980.0 -.97 -.08.97 1112.50 -7636.2 -1272.1 2070.0 -1.45 -.02 1.45 1113.00 -7711.9 -1259.3 2160.0 -2.37 -2.87 3.72 1113.50 -7778.4 -1444.2 2250.0.-1.77 -5.11 5.41

Double Theodolite Data - Shoreline Station - MYSIS Time Balloon.Position Wind Velocity x_ Y Z U V W 1200.00 -1336..2 79.3.2 1200.50 — 1205.1 34.2 77.6 4.37 -1.50 -.46 1201.00 -11-22.7 -26.9 1614.5 2.74 -2.03 -.25 1201.50 -1087.5 *4, 2 253.5.1.17 -2.24.01 1202 0.0 40:81. 2 -150.2 351.9.20 -1.86,.23 1202.50 -109-8.9 -190.7 452.3.59 -.429 1203.00 -1133.8 -227.2 551.0 -1.16 -1.21.24 12-03.50. 064181.4 -277.4 648.7 -1.58 -1.67.20 1204. 00' -1243.4 -342.5 753.7 -2.06 -2.16;.45 '1204.50' -.1330.0 -405.2- 865.3 -2.88 -2.09.67 1205.0-0 -1442.0O -447.7 966.1 -3.73 -1.41 ID30 1 205.50 -..1569. 2 -466.8 1055.8 -4.24 -.63 -.05.12016.00 -1713.9 -475.5 1149.3 -4.82 -.29.07 1206.50 -1873.0 -486.8 1249.5 -5.30 -> 7.28 1207.00. -2025.0 -506.6 1353.0 -5.06 -.65.40 12.Q7,*50 -2126.7 -526.6 1449.4 -3.39 -.66.16 1208.00.-2163..4 i-535.4 1533.4 -1.22 -.29 -.24 1208.50 -218~9.6 -538.7 1626.2.7 -1 0 1209,00 -"2230.1 -529.2 1729.8 -1.34 ~.31.40 1209.50 -2 26 2.9 -494.4 1817.2 -1.09 1.15 -.13 1210.00 -2322.9 -460.4 1902.3 -2.00 1.13 -.21 1210.50 -.2426.-5 -443.5 1995.8 -3.45.656.06 1211.000 -.2 54 5.5 -430.7 2085.5 -3.96.42 -0 5.1211.50 — 2672.2 -422.4 2170.8 -4.22.27 -.20 1212.00 -2791.6 -425.5 2239.6 -3.98 -.10 -.75 12112.50 -2917.6 -449.3 2308.5 -4.19 -.a79 -.74 1213.00 -3057.9 -501.7 2398.3 -4.67 -1.74 -.05 1213.50 -3179.5 -567.3 2488.8 -4.05 -2.18 -0 2 1214.00 -3316.0 -640.2 2580.5 -4.55 -2.43.00 1214.50 -3494.8 -737.1 2687.2 -5.96 -3.22.5 0 1215.00 -3656.9 -863.4 2798.1 -5.40 -4.21.64 1215.50 -3766.7 -1009.7 2895.5 -3.66 -4.87 49 1216.00 -3819.7 - I1 56A1'' 2969.7 -1.76 -4.88 -5 1216.50 -3869.6 -1304.4 3063.2 -1.66 -4.93.06 1217.00 -3948.6 - 1454...5 3189.4 -2.63 -5.00 1.15 1217.50 -4021.3 -1616'.5 3310.2 -2.42 -5.39.97 1218.00 -4019.5 -1774. 3 3367.4.06 -5.26 -1.14 1218.50 ~ -396I. 5 -19-14. 2 3 367.0 1.93 -4.66 -3.06 1219.00 -4003.7 -2099.4 3435.3 -1.40 -6.17 -76' 1219.50 -4091.2 -2311.0 3540.8 -2.91 -7.05.46 1220.00 -4114.3 -2501.2 3601.1 -.76 -6.33 -1.03

.Single Theodolite Data- MYSIS Balloon Position Wind Velocity Time X Y Z U V VT 1203.00.0.0.0 1203.50 -1494.7.01 90.0 3.65"- -1.19 3.84 1204.00 -1382.9 - 71.2 108.0 2.58 -2.42 3.54 1204.50 -1339.7 -145.4 270.0.87 -2.10 2.28 120,5.00 -1330.4 -197.4 -360,0 -.81 -.90 1.21 1205.50 -1388.3 -199.3 450.0 -1.12 -.91 1.45 1206.00 -1397.8 -252.2 540.0 -.35 -1.53 1.57 1206.50 - 1409.2 -291.3 630.0 -1.48 -2.31 2.74 1207.00 -1486.3 -390.7 720.0 -2.17 -2.56 3.35 1207.50 -1539.5 -444.7 810.0 -2.52 -1.96 3.19 1208.00 -1637.5.-508.0 900.0 -2.86 -1.94 3.46 1208.50 -1711.1 -561.2 990.0 -3.54 -1.76 3.95 120.9.00 -1849.9 -613.7 1080.0 -4.32 -1.72 4.65 1209.5Q -1970.4 -664.7 1170.0 -4.92 -1.~36 5.11 1210.00 -2145.2 -695.4 1260.0 -4.39 -1.04 4.51 1210.50 -2233.8 -726.9 1350.0 -3.05 -.52 3.10 1211.00 -2328.4 -726.4 1440.0 -2.18.05 2,.18 1211.50 -2364.8 -724.0 1530.0 -.33.71.78 1212.00 -'2348.4 -684.1 1620.0 -1.33 1.68 2.14 1212.50 -2444.5 -623.5 1710.0 -2.9'2.65 2.99 1213.00 -2523.5 -645.3 1800.0 -2.74.10 2.75 1213.50 -2609.1 -617.3 1890,0 -3.27 -.66 3.33 1214.00 -2719.5 -684.9 1980.0 -3.43 -2.10 4.03 1214.50 - 2815.2 -743.5 2070.0 -3.80 -2.06 4.32 1215.00 -2947.3 -808.5 2160.0 ).321 -3.41 4.69 1215.50 -3007.8 -948.3 2250.0 -1.26 -5.70 5.84

Single Theodolite Data - MYSIS Balloon Position Wind Velocity Time X Y Z U V VT 1347.00.0.0.0 1347.50 -6291.5 -54.3 90.0 3.36 -1.57 3.71 1348.00 -6206.5 -94.0 180.0 1.78 -1.90 2.60 1348.50 -6184.7 -168.3 270.0 -1.15 -2.96 3.18 1349.00 -6275.6 -271.5 360.0 -2.45 -2.70 3.65 1349.50 -6331.7 -330.6 450.0 -2.95 -1.50 3.31 1350.00 -6452.4 -361.6 540.0 -3.64 -.07 3.64 1350.50 -6550.1 -334.9 630.0 -2.64.61 2.71 1351.00 -6610.9 -324.7 720.0 -2.32 -.64 2.41 1351.50 -6689.5 -373.6 810.0 -.73 -3.01 3.10 1352.00 -6654.6.-505.6 900.0 -1.09 -3.78 3.93 1352.50 -6754.6 -600.4 990.0 -3.67 -2.69 4.55 1353.00 -6874.8 -666.8 1080.0 -8.28.53 8.29 1353.50 -7251.3 -568.9 1170,0 -10.30 5.58 11.72 1354.00 -7493.0 -331.8 1260.0 -7.67 9.10 11.90 1354.50 -7711.6 - 22.9 1350.0 -4.92 8.36 9.70 1355.00 -7788.4 169.6 1440.0 -1.01 3.58 3.72 1355.50 -7772.4 191.9 1530.0.47 -.46.66 1356.00 -7760.1 142.3 1620.0 -.29 -1.59 1.61 1356.50 -7789.5 96.8 1710.0 -.89 -1.55 1.79 1357.00 -7813.6 49.2 1800.0 -1.53 -3.33 3.67 1357.50 -7881.2 -103.2 1890.0 -3.15 -3.62 4.80 1358.00 -8002.8 -167.8 1980.0 -3.18 -1.69 3.60 1358.50 -8072.0 -204.5 2070.0 -3.17 -2.45 4.01 1359.00 -8193.1 315.0 2160.0 -4.85 -4.55 6.65 1359.50 -8362.9 68.5 2250.0 -3.41 -12.30 12.77

Double Theodolite Data - Shoreline Station Time.Balloon Position Wind Velocity x y z U V W 0600.00.0 274.3 7.6 0600.50 - 210.6 246.1 93.8 -7.02 -.93.17.0601.00 -~ 446.5 -19 1. 6 179.8 -7.86 - 1.81 —.17 0601.50 - 643.6 105.4 264.9 -6,56 - 2.87 -.21 0602.00 - 767.2 2.2 35400 -4.12 - 3.44 -.08 0602.50 -837.1 - 97.4 45-6.0 -2.32 - 3.32.38 0603.00 - 856.0 - 189.5 563.0 -.63 - 3.07.49 0603.50 - 851.4 - 281.4 665.0.15 - 3.06 035 0604.00 - 853.0 - 377.8 768.8 -.05 - 3.21.41 0604.50 - 858.6 - 4 822.2 870.5 -.1-8 - 3.48.34 0605.00 - 870.3 - 600.1 970.9 -.38 - 3.92.29 0605.50 -896.5 - 735.5 1078.2 -.87 - 4.51.52 0606.00 -932.2 - 880.3 1186.1 -1.."19 - 4.82.54 0606.50 971.5 -1035.4 1291.7 -1l.30 - 5.17.47 0607.00 -1011.4 -1218,5 1397.5 -1.32 -6,10.47 0607.50 -.1035.3 -J-I429.6 1490.6 -.79 7.03.05 0608.00 -1051.7 -1682.6 1596.1 -.54 -8.43.46 0608.50 -1063.0 -1948.4 1712.3 -.37 -8.85.82 0609,00 -1068.6 -2187.8 1816.0 -.18 -7.98.40 0609,50 -1093.8 -2426.3 1931.7 -.83 -7.95.80 0610.00 -1120.6 -2643.5 2036.1 -.89 -7.23.43 0610.50 -1131.1 -2798.2 2097,0 -.34 -5.15 -1.01 0611.00 -1146.2 -2963.7 2181.6 -.50 - 5.51 -.22 0611.50 -1167.8 -3211.7 2339.8 - 7172 -8.26 2.22 0612.00 -1152.7 -3413.7 2467.3.50 -6.73 1.20 0612.50 -1098.4 -3556.1 22549.1 1. 81, - 4,,74 -.32 061l3.00 -1040.0 -3786.1 2686.4 1.94 - 7.66 1.53 06113. 50 - 950.4 -4030,4 2819.9 2.98 8.14 1.40 0614.00 - 826.1 -4216.3 2897.9 4,14 - 6.19 -.44 0614.50 - 704.3 -4384.2 2958.3 4.06 5,59 -1.03 0615.00 - 570.7 -4544.,2 3002.3 4.45 -5,33 -1.58 0615.50, - 407.4 -4774.5 3 07 8.-5 5.44 -7.67 -.5 0616,00 -- 204.7 -5078.8 3207.7 6.75 -10.14 1.26 0616.50 32.5 -5398,2 3362.0 7.90 -10.64 2.09 0617.00 268.3 -5661.5 3492.6 7,86 - 8.77 1,30 0617.50 509.2 -5861.5 3582.7 8.02 - 6.66 -.04 0618.00 766.2 -6016.7 3632.6 8.56 - 5.17 — 1.38 0618,50 1009.6 -6092.9 3619.6 8.11 - 2,54 -3.48 0619.00 1215.7 -6175,9 3597.2 6.86 - 2.76 -3.79 0619.50 1404.0 -6360.1 3623,6 6.27 - 6.13 -2.17 0620.0 1623.0 — -- -671.4..i 3747.5- 7.30 -'I12,3)7 1.)08

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Velocit x y z U V W 0800.00.0 274.3 7.6 0800.50 -177.4 285.1 110.6 -5.91.35.38 080l.00 -397.9 310.0 219.5 -7.35.82.58 0801.50 -629.8 311.6 331.9 -7.72.05..69 0802.00 -799.6 248.3 436.1 -5.66 -2.10.42 0802.50 -885.8 138.0 529.6 -2.87 -3.67.06 0803.00 -92619.1 623.5 21.56 -3.96.08 0803.50 -963.7 -94.6 724.4 -1.03 -3.79.31 0804.00 -981.7 -204.1 830.9 -.60 -3.64.50 0804.50 -1000.5 -322.1 9.38. 2 -.62 -3.93.52 0805.00 -1026.6 -464.9 1042.0 -.87 -4.75.41 0805.50 -1057.6 -646.4 1144.3 -1.03 -6.05.36 0806.00 -1075.7 -867.6 1241.0 -.60 -7.37.17 0806.50 -1065.8 -1109.0 1329.1.33 -8.04 -.11 ~807.00 -1044.3 -1357.7 1427.3.71 -8.29.22 ~~807.50 -1020.4 -1586.5 1535.7 79 -.2.56 0808.00 -1000.5 -1774.6 1643.4.66 -6.27.54 0808.50 -1020.3 -1939.1 1752.0 -.66 -5.48.57 0809.00 -1084.5 -2086.5 1851.3 -2.13 -4.91.26 080.9.50 -1161.7 -2234.2 1949.3 -2.57 -4.92.21 08I0~~00 -1223.2 -2395.5 2047.1 -2.04 -5.37.2 0810.50 -1253.0 -2552.5 2127.4 -.99 -5.23 -.36 0811.00 -1265.4 -2723.6 2214.1 -.41 -5.70 -.15 0811.50 -1263.6 -2923.7 2313.6.05 -6.67.26 0812.00 -1306.8 -3322.1 2528.1 -1.43 -13.28 4.10 0812.50 -1348.6 -3726.8 2734.6 -1.39 -13.48 3.83 0813,,00 -1253.7 -3749.4 2677.3 3.16 -.a7 5 -4.95 0813.50 -1149.8 -3833.3 2647.4 3.46 -2.79 -4.04 0814.00 -1107.1 -4213.5 2798.1 1.42 -12.67 1.97 0814.50 -1013.8 -4503.0 2880.2 3.10 -9.64 -.31 0815.00 -859.9 -4667.2 2879.0 5.13 -5.47-30 0815.50 -701.6 -4928.0 2944.9 5.27 -8.69 -.85 0816.00 -558.2 -.5289.6 3081.6 4.77 -.12.05 1.51 0816.50 -411.9 -5560.2 3167.1 4.87 -9.02 -.20 0817.00 -257.7 -5735.7 3188.8 5.13 -5.84 -2.3 2 0817.50 -99.1 -6059.5 3278.1 5.28 -10.79 -.07 0818.00 54.6 -6422,6 3393.0 5.12 -12.10.78 0818.50 190.5 -6671.2 3455.4 4.52 -8.28 -.96 0819.00 311.1 -6914.2 3515.1 4.02 -8.10 -1.05 0819.50 421.5 -7018.2 3506.9 3.68 -3.46 -3.32 0820.00 522.3 -6979.1 3429.1 3.36 1.30 -45.64

Double Theodolite Data - Shoreline Station T i -L-e ]Balloon Position Wind Veloct x y z U V W 0830.00.0 274. 3 7Th6 0830. 50 -167.1 286.8 113.1 -5. 57 Al1.46 0831.00 -357.7 302.2 2.09.2 -6.35.51.15.0831.50 -565.2 306.1 299A0" -6.91.12 -.04 0832.00 -744.5 275.2 394.'7 -5,97 -1.02.12 0832.50 -3E.3 205.9 4973-3.69 -2.30.3.0833.00 -902.2 122.7 599,7 -1.56 -2.77.36 0833.50 -909.6 35.8 698.8 -.24 -2.89.25 0834.00 -901.3 -57,3 797,5.27 -3.10.24 0834.50 -899.4 -147.4 895.7.06 -3.00.22 0835.00 -910.0 -237.7 992.2 -.35 -3.00.16 0835.50 -930.0 -359.1 1088.1 -.66 -4.04.15 0836K00 -948.8 -536.1 1186.1 -r,.62 -5.90.21 0836.5 0 -944.7 -757.8 1299.5.13 -7.39.06 0837.00 -918.7 -999.3 1369.1.86 -8.04 -.0O6 0837.50 -890.3 -1239.3 1473,8.94 -8.00.44 0838.00 -860,8 -1457.1 1594.5.98 -7.25.97 0838.50 -835.2 -1629.7 1703.7.85 -5.75 059 0839.00 -840.1 -1757.0 1791.3 -.16 -4.24 -i,13 0839.50 -884.6 -1873.6 1874,5 -1,48 -3.88 -.27 0840.00 -944.6 -2011,3 1966.4 -1.199 -4.58.01 0840.50 -968,8 -2094.2 1997.6 -.80 -2.76 -2.00 0841,,00 -975,3 -2194.0 2032.9 -.21 -3.32 -1.86 0841.50 -1014.3 -2463.1 2200.5 -1.30 -8,96 2.53 0842.00 -1037,8 -2738.2 2355.3 ~:~78 -9.16 2.11 0842.50 -1048.0 -2982.2 2470.1 -.33 -8.13.77 0843.00 -.1059.1 -3256.9 2601.0 -.36 -9.15 1.31 0843.50 -1025.1 -3484.9 A267 8.6 1.13 -7.60 -.46 0844.00 -969.4 -3755.4 2768.1 1,85 -9.01 -.06 0844,50 -890.8 -4043.3 2865.1 2,62 =9.59.18 0845.00 -C&63.0O -4235.0 2 9 02,.5 4.25 -6.38 -1.80 0845.50 — 639.9. -4437.,4 2964.,7 4.10 -7.41 -.97 0846.00 -541,,9 - 4.73)0.7 3064.5 3.26 -9,77.27 0846.50 -447.0 -5055.2 3159.7 3,16 -10.15.12 0847.00 -360.3 -5397.8 3273.8 2.88 -11.41.75 0847.50 -291.1 -5797.5 341.2. 7 1.30 -13.32 1.57 0848.00 -2222.2 -6103.7 3493.3 2.,29 -10.20 -.35 0848.50 -131.9 -6324.2 3534.3 3'O"01 -7.34 -1.68 0849.00. -31,5 — 67483,5 3697.3 3.34 -14.,47 2.38 0849.50 77.6 -7215.1 3876.2 3.64 -15.22 2..91 0850.00 202.5 -7352.2 3894.6 4.16 -4.56 -2.43

Double Theodolite Data - Shoreline station Time, Balloon Position Wind Velocity x y z U V W 0930.00.0 274. 3 7.6 ~0930.50 -120.1 274. 3 98.0 -4.00 -A8-.b 3 0 931.00 -249.8 25 2. 9 19 2. 3 -4. 32 -,.42.09 0 931. 50 -384.1 241.9 295.0 -4.47 -3.3 7 0 932.00 -5lp.1 235. 7 415.9 -4. 39 -.20.98 0 932.,50 -647.8 228. 1 544.6 -4. 38 -25 1. 24 0 933.00 -777. 9 20 3. 5 663. 3 -4. 33 -.81. 9W 0 933.,50 -878.8 149. 3 771.1 -3. 36 -1.80.54 0934.00 -927.7 77.7 869.0 -1.63 -2.38.21 0934.50 -944.6 ~ '-8. 3 958.6 -.56 -2.31 -.05 0935.00 -963.1 -60.1 1049.2 -.61 -2.28 -.02 0935.50 -988.3 -150.5 1145.2 -.84 -3.01.15 0936.00 -1005.0 -275.4 1241.3 -.55 -4.16.15 0936.50 -1003.7 -422.7 1332.0.04 -4.90 -.02 0937.00 -988.0 -587.5 1425.3.52 -5.49.06 0937.50 -9/71.9 -764.7 1530.7.53 -5.90.46 0938.00 -963.5 -922.6 1632.5.28 - 5.-i2 6.34 0938.50 -977.2 -1047.0 1733.9 -.45 -4.14.33 0939.00 -1018.6 -1137.5 1837.3 -1.37 -3.01.40 0939.50 -1065,0 -1199.8 1917.7 -1.54 - 2'!.O7 -.36 0940.00 -1114-.4 -1284.2 1993.4 -1,64 -2.81 -.52 0940;,.50 -1173.1 -1411.5 2084.3 -1.95 -4.24 -.02 0941.00 -1271.1 -1613.3 2246.5 -3.26 -6.72 2.35 0941.:50 -1364.5 -1838.8 2416.4 -3.11 -7.51 2.61 0942.00 -1372.5 -1970.0 2453.5 -.26 -4.37 -1.80 0942.50 -1372,4 -2097.3 2480.3.00 -4.24 -2..1,5 0943.00 -1401.3 -2298.7 2571.7 -.96 -6.,71 -.00 0943.50 -1409,3 -2527.4 2.654.1 -.26 -7.62 -.30 0944.,00 -1390.7 -2766.0 2720.8.62 -7.95 -.82 0944.,50 -1362.0 -3041.0 2813.7.95 -9.16.05 0945.00 -1334.8 -3353.2 2941.9.90 -10.40 1.22 0945.50 -1297.2 -3624.'O3 3043.7 1.25 -9.06.34 0946.00 -1260.4 -3864.1 3123.6 1.22 -7.95 -.38 0946.50 -1243,.5 -4131.6 3222.5.56 -8.91.24 0947.00 -1234.1 -4469.2 3370.7.31 -11.25 1.89 0947,:50 -1200.7 -4828.3 3535.0 1.11 -11.97 2.42 0948.,00 -11391-,.7 -5135.1 3651.3.2.03 410,22.82 0948.,50 -1058,2 -5386.4 3722.3 2.71 -8.37 -.68 0949.,00 -929,4 -5511,2 3720.6 4.29 -4,15 -3.10 0949.50 ~ -767.9 -5649.2 3737.1 5.38 -4.59 -2.49 0950.c00 -612.5 -6002.6 3888.0 5.18 -11.77 1,98

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V W 1000.00.0 274.3 7.6 1000.50 -87.8 242.2 138.5 -2.92 -1.06 1.31 1001.00 -188.9 213.5 284.8 -3.36 -.95 1.83 1001.50 -284.6 198.2 455.1 -3.19 -.50 2.62 1002.00 -361.0 202.6 621.6 -2.54.14 2.50 1002.50 -424.0 228.4 751.2 -2.10.85 1.27 1003.00 -473.9 256.7 856.4 -i..94.45 1003.50 -512.7 258.0 969.5 -1. 29.04.72 1004.00 538.7 217.8 1080.0 -.86 -1. 34.63 1004.50 -548.3 133.5 1163.2 -.32 -2.80 -.27 1005.00 -559.3 19.0 1248.0 -.36 -3.81 -.21 1005.50 -579.7 -109.5 1349.6 -.67 -4.28.33 1006.00 -601.2 -243.2 1447.2 -.71 -4.45.20 1006.50 -623.7 -367.4 1540. 4 -.74 -4.13.05 1007.00 -648.9 -466.2 1636.3 -.84 -3.29.15 1007.50 -682.2 -526.6 1732.3 -1.10 -2.01.15 1008.00 -732.7 -569.2 1820.9 -1.68 -1.42 -.09 1008.50 -802.2 -641.9 1907.0 -2.31 -2.42 -.17 1009.00 -883.9 -751.5 1997.1 -2.72 -3.65 -.04 1009. ri,0..... 3. -O SE.2.. 2 '-97 -4.46.25 1(10.,00 — 1059.4 -1046. 1 2205.0 -2.87 -5.35.57 1010.50 -1133.2 -1226.5 2:310.4 -2.45 -6.01.46 1011.00 -1200.6 -1404.1 2412.6 — 2.24 5.91.35 1011.50 -1266.0 -1580.5 2520.4 -2.18 -5.88.54 1012.00 -1319.8 -1770.3 2618.1 -1.79 -6.32.20 1012.50 -1358.3 -1978.7 2704.2 -1.28 -6.94 -.18 1013.00 -1397.6 -2241.3 2832.8 -1.30 -8.75 1.23 1013, 50 -1404.4,-210 9 2959.4.22 -8.98 1. 1.7 1014.00 -1350. 7 -271'9. 7 3015 5 1.7 -6. 96 -1 13 1 014.50 -1 310.4 -2959.7 3109.6 1.34 -8.00. (3 1015. 00 -1314.2 -3247.9 3259.0 -.12 -9.60) 1. 93 1015.50 -1303.6 -34/99.0 3358.3.35 -8.37.26 1016.00 -1262.2 -3747.3 3439.7 1.38 -8.27 -.33 1016.50 -1211.1 -4018.0 353 3.3 1.70 -9.02.07 1017.00 -113. -4234.9 357. 2.4:0 -7.22 -1.78 1017.50 -1051.4 -44, o4.1 i 3.33 7 2.:91. 0 -. 96 IO18.00 -971.2 -4890.9 3828.8. 2.! - 3.45 1018.50 -857.8 -5233.7 3981.1.77 -11. ' 2.02 1019.00 -688.4 -5342.1 3960.9 5.64 -3. 1 -3.72 1019.50 -503,3 -5441.7 3,937.4 6.16 -3.32 3.83 1020.00 -333.1 -5732. Li 4050.2" 5.67 -9.7.70

Double Theodolite Data - Shoreline Station Time, Balloon Position Wind Veloct X Y Z tJ Vs W 1030.00.0 274.3 7.6 1030.50 -59.7 244.7 124.6 -1.99 -.098.85 1031.00 -137.5 199.7 254.2 -2.59 -1.50 1.27 1031.50 -218.3 157.4 383.9 -2.69 -1.41 1.27.1032.00 -287.2 121.2 508.1 -2.29 -1.20..1.09 1032.50 -352.2 93.0 634.7.-2.16 -.93 1.17 1033.00 -429.1 86,6 772.5 -2.56 -.21 1.54 1033,50 -515.0.92.2 917.5 -2.86.18 1.78 1034.00 -586.7 77.9 1042.1 -2.39 -.47 1.10 1034.50 -638.6 30.2 1136.1 -1.72 -1.58.08 1035.00 -685.6 -41.2 1223.3 -1.56.-2.38 -.14.1035.50 -736.4 -116.6 1317.8 -1.69 -2.51.10 1036.00 -794.4 -189.0 1436.3 -1.93 -2.41.90 1036.50 -844.0 -261.4 1559.0 -1.65 -2.41 1.04 1037.00 -875.7 -315.0 1652.4 -1.05 -1.78.06 1037.50 -918.0 -343,1 1742.9 -1.40 -.93 -.03 1038.00 -985.8 -373.2 1835.7 -2.26 -1.00.04 1038.50 -1075.9 -431.0 1925.0 -3.00 -1.92 -.07 1039.00 -1178.8 -513.0 2016.3 -3.43 -2.73 -.00 1039.50 -1283.1 -609.6 2109.8 -3.47 -3.22.06 1050.00 -1385.3 -728.4 2212.5 -3.40 -3.96.37 1040.50 -1481.8 -868.4 2318.0 -3.21 -4.66.46 1041,00 -1574.6 -1015.1 2421.3 -3.09 -4.88.39 1041.50 -1666.5 -1169.5 2521.8 -3.06 -5.14.30 1042.00 -1755.5 -1340.2 2617.7 -2.96 -5.68.14 1042.50 -1845.4 -1537.4 2728.5 -2.99 -6.57.64 1043.00 -1917.,0 -1763.6 2854.5 -2.38 -7.54 1.15 1043,,50 -1942.1 -1994,6 2961,0 -.83 -7.69.50 1044.00 -1941.8 -2219.3 3049.7.00 -7.49 -.09 1044.50 -1978.5 -2490.9 3192.3 -1.22 -9.05 1.70 1045.00 -2029,7 -2768.2 3347.1 -1.70 -9.24 2.11 1045.,50 -2004.5 -2937.6 3380.3.83 -5.64 -1.94 1046.00 -1964.9 -3106.3 3402.8 1.31 -5.62 -2.29 1046.50 -1979.6 -3380.4 3534.5 -.48 -9.13 1.34 1047.00 -1968.3 -3655.1 3659.5.37 -9.15 1.12 1047.50 -1882.9 -3854.5 3703.4 2.84 -6.64 -1. 58 1048.00 -1767.5 -5067.4 3754.3 3.84 ~-7.09 -1.34 1048.50 -1663.4 -4372.9 3884.5 3.46 -10.18 1.29 1049.00 -1540.4 -4666.1 4002.9 4.10 -9.77.89 1049.50 -1388.1 -4934.1 4086.3.5.07 -8.93 -.26~ 1050.00 -1251.0n -5306.3 4241.8 4.5 M7 -12.40n 213 I

Double Theodolite Data - Shoreline Station Time, Balloon Position Wind Velocity N Y Z U V W 1100.00.0 274.3 7.6 1100.50 10.4 219.4 137.1.34 -1.82 1.26 1101.00 -13.2 167.0 272.0 -.79 -1.74 1.44 1101.50 -82.7 131.0 430.1 -2.31 -1.20 2.22 1102.00 -165.4 114.6 587.2 -2.75 -.54 2.18 1102.50 -240.1 99.7 723.7 -2.49 -.49 1.50 1103.00 ~ -316.7 59.0 863.2 -2.55 -1.35 1.60 1103.50 -406.7 4.7 1003.1 -2.99 -1.81 1.61 1104.00 -501.5 -35.0 1119.4 -3.16 -1..32.82 1104.50 -580.0 -66.8 1211.4 -2.61 -1.06.01 1105.00 -644.4 -109.2 1289.4 -2.14 -1.41 -o44 1105.50 -701.8 -162.6 1369.9 -1.91 -1.77 -.36 1106.00 -750.8 -215.7 1464.4 -1.63 -1.77.10 1106.50 -794.4 -253..3 1559.0 -1.45 -1.25.10 1107.00 -835.5 -266.3 1665-1.37 -o43 -O. 13 1107.50 -867.7 -253.4 1,723.7 -1.07.4.2 -.47 1108.00 -906.2 -238.5 1804.8 -1.28.49 -.34 1108.50 -984.1 -261.6 1910.4 -2.59 -.77.47 1109.00 -1087.8 -321.4 2009.7 -3.45 -1.99.26 1109.50 -1195.5 -392.8 2094.6 -3.58 -2.38 -.21 1110.00 -1306.4 -472.0 2182.4 -3.69 -2.63 -.12 1110.50 -1421.5 -565.2 2270.6 -3.83 -~.l0 -210 1111.00 -1547.7 -671.0 2364.2 -4.20 -3.52.07 1111.50 -1678.7 -792.4 2475.1 -4.36 -4.04.64 1112.00 -.1811.1 -940.9 2607.7 -4.41 -4.94 1.37 1112.50 -1935.7 - 110 8- 0 2733.3 -4.15 -5.56 1.13 1113.00 -2030.1 -12 7 229 2824.1 -3.14 -5.49 -.02

Double Thteodoiite Data - Sftoreline Station Time Balloon Position W ind Veloct x y z U V W 1130.00. 0 274. 3 7.6 1130. 50 84.5 250.6 127. 2 2.81 -.78.94 1131.00 138.8 213.5 247.4 1.81 -1.23.95 1131.50 144.4 179.0 364.4.18 -1.14.85 1132.00 82,5 163.4 474.4 -2.06 -.51.62 1132.,50 -13.0 157.3 581.1 -3.18 -.20.50 1133.00 -108.6 151.2 687,7 -3.18 -.20.50 1133.50 -204.3 145,1 794.3 -3.18 7.20.50 1134.00 -299,9 139.0 901.0 -3.18 -.20.50 1134.50 -395.5 132.9 1007.6 -3.18 -.20.50 1135.00 -491.1 126.8 1114,2 -3.18 -.20.50 1135.50 -586.1 114.4 1228.1 -3.16 -.41.74 1136.00 -674.0 84.4 1348.7 -2.93 -1,00 097.1136.50 -736.3 44.3 1462,1 -2.07 -1.33.73 1137.00 -766.1 18.5 1566.1 -.99 -.85.042 1137.50 -784.1 15.8 1663.8 -.60 -.09.20 1138.00 -806.4 29.1 1761.4 -.74.44?'2 0 1138.50 -839.1 49.9 1858.3 -1.08.69.18 1139.00 -895.3 60.2 1944.8 -1.87.34 -41 1139.50 -983.9 43.5 2035.1 -2.95 -.55 -.03 1140.00 -1097.0 8.3 2133.4 -3,76 -1.17.22 1140.50 -1213,1 -30.8 2212.3 -3.86 -1.30 -.041 1141.s00 -1331.4 -.79. 2 2278.0 -3,94 -1.61 -.85 1141.50 -1473.2.. —4,51.0 2367.3 -4.72 -2.39 -.07 1142~,00 -1614,,4 — 245.4 2466.8 -4.70 -3.14.26 1142.50 -1741.0 -— ~353.'4 2555.6 -4.21 -3.59 -.08 1143,,00 -1884.2 -473.5 2653.3 -4,77 -4.00.21 1143.50 -2013.6 -601.2 2736.2 -4.31 -4.25 -.28 1144,,00 -2111.4 -746.2 2805.9 -3.25 -4.83 -.72 1144.50 -2210.2 -918.6 2906.1 -3.29 -5.74.29 1145.00 -2288.6 -1096.6 3014.6 -2,61 -5.89.56 1145.50 -2328.8 -1252.9 3106.2 -1,34 -5.24.00 1146.00 -2360.4 -1390,3 3192.1 -1.05 -4.58 -.18 1146.50 -2391.7 -1529.6 3276.3- -1,04 -4.64 -.24 1147.00 -2401.1 -1677.3 3335.0 -.31 -4.92 -1.08 1147.50 -2415,7 -1844,0O 3390..O -.48 -5.55 -1.21 1148.00 -2472.2 -2060.8 3493.5 -1.88 -7.22.40 1148.50 -2518,1 -2294,7 3603.9 -1.53 v. 7.79.63.1149.~00 -2.535.,2 -2527.5 3717,7 -.56 -7.76.74 1149.50 -2585.0 -2808.9 3909.2 -1.66 -9.38 3.33

Double Theodolite Data - Shoreline station Time Balloon Position Wind Velocity x y z U V W 1330.00.0 274.3 7.6 1330.50 92.1 154.2 105.3 3.07 -4,00.21 1331.00 185.9 49.1 199.0 3.12 -3,50.0-7 1331.50 253.8 -28.5 293,6 2,26 -2.58.10 1332.00 257.9 -69.4 395.0.13 -1.36.33 1332.50 197.3 -78.2 499.7 -2.02 -.29.44 1333.00 99.2 -71.3.""599o2 -3.26.22.26 1333.50 -17.0 -64.7 691.3 -3.87.22.02 1334.00 -139.4 -.61.1 780.7 -4.07.11 -.06 1334.50 -261.7 -57.6 870.2 -4.07 I.11 -.'06 1335.00 -384.1 -54.,1 959.6 -4.07.11 -.06 1335.50 -520.5 -43.6 1053.1 -4.54.35.06 1336.00 -685.6 -15.7 1151.9 - 5' 5 0.92.24 1336.50 -868.8 21.3 1248.5.-6. 10 1.23.17 1337.00 -1058,0 53.2 1340.6 -6.30 1.06.02 1337.50 -1248,9 83.9 1428,4 -6,36 1.02 -.12 1338.00 -1427.1 118.7 1511.0 -5.93 1,15 -.29 1338.50 -1565.6 157.9 1602.0 -4.61 1.30 -.01 1339,00 -1658.1 205.9 1711.8 -3.108 1.59.61 1339.50 -1715,1 265.5 1816.7 -1. 90 1.98.44 1340.00 -1759,8 330.3 1907.2 -1,48 2.16 -.02 1340.50 -1829,6 386.4 2005,2 -2,32 1.87.21 1341.,00 -1927.3 425.6 2109.3 -3.25 1.30.42 1341.50 -2037.1 438,7 2200.7 -3.66.343 -.00 1342.00 -2166.9 435.9 2290.8 -4.32 -.09 -.04 1342.50 -2317.9 437.2 2401.7 -5.03.04.64 1343.00 -2446.3 438.7 2505.6 -4.27.05.41 1343~,50 -2554.3.420.5 2598.8 -3.60 -.60.05 1344.00 -2665.0O 359.8 2697.6 -3,69. -2,,02.24 1344.50 -2747.3 2 64. 8 2,798.4 - 2..74ZP -3.16.04 1345.00 -,279,0.0O 156.8 2.884. 6 -1.42 -3. 59.09. 1345.50 -.2810..9- 3.2.7 2985.6 -.69 -4..13.32 1346.00 -2.844.1I -118.4 3 0918'.3 -1. 10. -5.04.70 1346.50 -289,9,.4 -.291.7 3215.8 -1.84 -5.77.86 1347.00 -.2945..6 -474.3.B 3 3 19.3 -1.,54. -6. 10 -.40 1347.50 -2958.4 -6.5,9'.,1 3414..2 -.42 -6.14.1 1348.00 -2-93 2.7 -'8 35..0 3505.3..85 -5.86 -0 1 1348.50 -2890.9 -10 14'.4 31596. 3 1,.39 -:5.9.7 -01 1349.00 -2843.0 -12 05.;8 3,683.5 1. 59 -6. 38 -14 1.349.50 -2797.9 -1413.9 378:5..9 1. 50 -6'.9 3.36 1350.00 -2792.8 -1651.9 3951.2.17 -7.93 2.46

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Veloct x Y Z U V W 1400.00.0 274.3 7.6 1400.50 91.0 154.2 107.3 3.03 -4.00.27 1401.00 171.9 66.0 202.3 2.69 -2.94.11.1401.50.201.0 6.9 300.2.96 -1.96.21 1402.00 161.4 -36.1 400.2 -1.31 -1.43.28 1402.50 79.6 -66.7 493.5 -2.72 -1.01.06 1403.00 -19.2 -87.4 577.9 -3.29 -.68 -23 1403.50 -125.9 -113.4 667.2 -3.55 -.86 -.07 1404.00 -238.4 -156.9 773.9 -3.74 -1.45.50 1404.50 -351.6 -205.1 888.2 -3.77 -1.60.76 1405.00 -470.8 -239.5 997.7 -3.97 -1.14.60 1405.50 -606.4 -254.9 1102.5 -4.51 -.51.44 1406.00 -755.5 -252.5 1204.8 -4.96.07.36 1406.50 -918.0 -232.7 1299.4 -5.41.65.10 1407.00 -1087.3 -200.3 1386.6 -5.64 1.08 -.14 1407.50 -1235.6 -166.0 1471.3 -4.94 1.14 -.22 1408.00 -1331.8 -126.5 1558.6 -3.20 1.31 -.13 1408.50 -1372.6 -75.2 1655.4 -1.36 1.70.17 1409.00 -1381.0 -21.7 1755.0 -.28 1.78.27 1409.50 -1384.8 34.7 1846.7 -.12 1.88.00 1410.00 -1413.3 102.6 1942.3 -.95 2.26.13 1410.50 -1474.2 177.0 2047.4 -2.02 2.47.45 1411.00 -1553.2 251.2 2149.1 -2.63 2.47 034 1411.50 -1648.3 313.2 2247.6 -3.16 2.06.23 1412.00 -1765.4 352.9 2354.2 -3.90 1.32.050 1412.50 -1892.7 379.0.2469.7 -4.24.86.80 1413.00 -1998.0 401.2 2569.0 -3.50.73.26 1413.50 -2093.8 406.3 2656.7 -3.19.17 -.12 1414.00 -2202.6 363.7.2756.1 -3.62 -1.41.26 1414.50 -2299.0 274.4 2863.7 -3,21 -2.97.54 1415,00 -2294.1 174,1 2892.2.16 -3.34 -2.09 1415.50 -2225.9 56,9 2874,1 2.27 -3.90 -3.65 1416.00 -2287.4 -105.6 302-3,7 -2.05 -5.42 1.93 1416.50 -2416.8 -287.1 3246.7 -4.31 -6.04 4.38.1417.00 -2474.8 -467.4 3366.8 -1.93 -6. OiL.95 1417.50 -2508.8 -665.3 3474,6 -1. 13' -6.59.54 1418.00 -2524.0 -868.2 3601.1 -.50 -6.76 1.16 1418,50 -2506.5 -1068.7 3709.3.58 -6.68.55 1419.00 -2478.3 -1276,4 3802.0.94 -6.92.04 1419.50 -2436.7 -1482.8 3880.7 1.38 -6.88 -.42 1420.00 -2405,,8 -1696.0 3990.1 1.03 -7.10.60

Double Theodolite Data -Shoreline Station Time Balloon Position Wind Velocity x y z U V W 1430.00.0 274. 3 7.6 1430.50 99. 3 121.2 108.7 3.31 -5.10.32 1431.00' 180.9 2.6 204.5 2.71 -3.95.14 1431.50 203.8 -70.8 301.4.76 -2.44.17 1432.00 163,3 Ik-l0 9.0 402,1 -1.34 -1,27.30 1432.50 82,0 -130.7 504.6 -2.71 -.72.36 1433.00 -21.0 -148.5 605.7 -3.43 -.59.32 1433.50 -139.9 -168.0 712.5 -3.96 -.64.51 1434.00 -277,1 -184.8 829.7 -4.57 -.56.85 1434.50 -420.8 -187.0 943.6 -4,79 -.07.75 1435.00 -569.1 -175.9 1053.9 -4.94. 37.62 1435.50 -733.7 -160.0 1166,9 -5.48.53.71 1436.00 -913.3 -142.6 1275.5 -5.98 057.57 1436.50 -1092.2 -116.4 1381.0 -5.96.87.46 1437.00 -1234.0 -61.8 1488.2 -4.72 1.81.52 1437.50 -1305,8 22.3 1595.2 -2.39 2.80.51 1438.00 -1332.8 114,0O 1709.4 -.89 3.05.75 1438.50 -1352.7 203.9 1823.0 -.66 2.99.73 1439.00 -1384.3 298,2 1922.9 -1.05 3.14.28 1439.50 -1445.0 392.3 2023.3 -2.02 3.13.30 1440.00 -1523.8 481,1 2123.3 -2,62 2.95.28 1440.50 -1622.2 566.1 2225.6 -3.28 -2.83.36 1441,00 -1745.3 648.5 2332.0 -4.10 2.74.49 1441.50 -1862,1 724.9 2424,2 -3.89 2.54.02 1442.00 -1960.4 787.1 2517.8 -3.27 2.07.07 1442.50 -2056.7 817,6 2630,5 -3.20 1.01.70 1443.00 -2180.0- 794.5 2778.3 -4,11 -.76 1.87 1443.50 -2291.3 720.2 2930.4 -3.70 -2,47 2.02 1444,,00 -2307.1 606.3 3013.0 -.52 -3.79 -.29 1444.50 -2271.8 461,2 3060,6 1.17 -4.83 -1.45 1445.00 -2272.0 298.0 3138.0 -.00 -5.43 -.46 1445.50 -2311.0 127,6 3247,2 -1,30 -5.68.59 1446.00 -2347.1 -49.0 3360.3 -1.20 -5,88.72 1446.50 -2353.3 -238.3 3458.9. -.20 -6.31.23 1447.00 -2358.6 -442,5 3583,2 -.17 -6.80 1.09 1447.50 -2352.6 -651.1 3700.7.19 -6.95.86 1448,,00 -2324.1l -860.8 3787,1.95 -6.98 -.16 1448.50 -2312.5 -1080.4 3911.3.38 -7.31 1.09 1449.00 -2270,2 -1285.2 4021.2 1.41 -6,82.61 1449.50 -2159.1 -1457.5 4066.1 3.70 -5.74 -1.55 1450.,00 -2024.6 -1618,2 4092.4 4.48 -5.35 -2.17

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Velocy x y z U V W 1800.00.0 274.3 7.6 1800.50 104.6 111.0 101.1 3.48 -5.44.06 1801.00 193.1 -26.0 193.8 2.95 -4.56.04 1801.50 229.2 -105.9 285.0 1.20 -2.66 -.00 1802.00 205.8 -150.5 375.8 -.77 -1.48 -.02 1802.50 151.6 -188.5 468.1 -1.80 -1.26.03 1803.00 82.1 -218.0 563.5 -2.31 -.98.13 1803.50 3.5 -233.3 662.4 -2.62 -.51.24 1804.00 -81.7 -232.3 758,2 -2.84.03.14 1804.50 -185,1 -219.7 851.3 -3.44.42.05 1805.00 -310.9 -206.1 949.9 -4.19.45.23 1805.50 -452.8 -190.8 1050.0 -4.72.050.29 1806.00 -605.7 -166.6 1146.7 -5.09.80.17 1806.50 -763.6 -136.4 1239.1 -5.26 1.00.02 1807.00 -922.6 -102.3 1329.1.-5.29 1.13 -.04 1807.50 -1085.2 — 61.*9 1422.5 -5.41 1.34.06 1808.00 -1251.8 -16.3 1516.2 -5..55 1.51.07 1808.50 -1409.9 38.2 1604.8 -.5.27 1.81 -.,09 1809."00 -1551.5 106.0 1692.0 -4.71 2.26 -..14

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V W 1830.00.0 274.3 7.6 1830.50 57.4 123.1 106.3 1.91 -5.03.24 1831.00 98.4 30.7 203.8 1.36 -3.08.20 1831.50 86.3 -13.5 296.0 -.40 -1.47.02 1832.00 30.6 -42.0 384.1 -1.85 -.95 -.11 1832.50 -43.6 -66.9 477.7 -2.47 -.82.07 1833.00 -131.2 -81.7 577.5 -2.91 -.49.27 1833.50 -226.3 -80.4 679.2 -3.16.04.34 1834.00 -324.4 -66.6 788.1 -3.27 o45.58 1834.50 -419.0 -46.9 895~6 -3.15.65.53 1835.00 -512.9 -24.5 988.1 -3t13.74.03 1835.50 -617.9 -.8 1079.9 -3.50.78.01 1836.00 -735.2 23.3 1176.6 -3.90.80.17 1836.50 -863.3 51.8 1268.3 -4.26.95.00 1837.00 -1008.5 86.9 1356.7 -4.84 1.16 -. 10 1837.50 -1174.9 125.2 1448.1 -5.54 1.27.00 1838.00 -1330.0 169.2 1542.3 -5.17 1.46.09 1838.50 -1440.5 235.3 1650.8 -3.68 2.20.56 1839.00 -1488.4 335.1 1776.8 -1.59 3.32 1.14 1839 50 -1453.8 454.0 1888.6 1.15 3.96.68 1840.00 -1379.4 570~6 1990.7 2.48 3.88.35 1840.50 -1318.5 682.7 2097.7 2.02 3.73.51 1841, 00 -1270 o 1 795.9 2193.3 1.61 3.77.13 1841.50 -1234.7 889.8 2275.1 1.17 3.13 -.32 1842.00 -1234.2 951.2 2367.7.01 2.04.04 1842.50 -1272.8 985.2 2482.2 -1.28 1.13.76 1843. 00 -1310.4 978.7 2584.4 -1.25 -.21.35 1843.50 -1316.6 929.7 2661.o2 -220 -1.63 -.48 1844.00 -1322.0 870.7 2764.6 -.18 -1.96.39 1844.50 -1342 o 2 821.4 2905.0 -.67 -1.64 1.63 1845.00 -1342.0 766.6 3028.4 o.00 -1.82 1.06 1845.50 -1324.9 703. 7 3142.4.56 -2.09.75 1846.00 -1313.8 644.6 3266.5.37 -1.97 1.09 1846.50 -1304.0 589.9 3384.5 o 32 -1.82.88 1847.00 -1288.6 539.0 3502.8.51 -1.69.89 1847.50 -1262.7 490.6 3636.1.86 -1.61 1.39 1848.00 -1216.2 435.1 3766.2 1.55 -1.84 1.28 1848.50 -1147.1 367.9 3876. 6 2.30 -2.24.62 1849,00 -1078.2 294.9 4003.0 2.29 -2.43 1.16 1849.50 -1005.5 217.7 4135.3 2.42 -2.57 1.36 1850.00 -906.0 136.2 4224~3 3.31 -2.71 -.08

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Veloct x y z U V W 1900.00.0 274.3 7.6 1900.~50 10.8 171.9 105.8.36 -3.41.22 1901.100 -22.5 102.8 197.0 -1.11 -2.30 -.00 1901.50 -101.6 63.2 ~263-2.63 -1.32 -.07 1902.00 -204.1 37.9 375.1 -3.41 -.84 -.08 1902.50 -317.4 19.1 462.5 -3.77 -.62 -.13 1903.00 -435.2 3.4 549.1 -3.92 -.52 -.16 1903.50 -553.6 -9.2 635.3 -3.94 -.42 -.17 1904.00 -673,1 -18.9 721.2 -3.98 -.32 -.18 1904.50 -797.1 -28.3 808.2 -4.13 -.il -.14 1905.00 -949.0 -35.8 915.7 -5.06 -.25.53 1905.50 -1106.6 -32.9 1026.1 -5.25.09.63 1906.,00 -1224.0 -13.8 1099.3 -3.91.63 -.60 1906.50 -1342.7 13.7 1167.7 -3.95.91 -.76 1907.00 -1490.4 40.1 1255.3 -4.92.88 -.12 1907.50 -1631.5 75.6 1354.1 -4.70 1.18.24 1908.00 -1718.0 137.1 1453.0 -2.88 2.04.24 1908.50 -1739.8 221.1 1538.7 -.72 2.80 -.19 1909.00 -1720.1 325.4 1622.5.65 3.47 -.25 1909.50 -1663.4 451.5 1711.8 1.89 4.20 -.07 1910,00. -1583.2 581,7 1806.8 2.67 4,.34.12 1910.50 -1501.0 700.3 1903.9 2.74 3.95.18 1911.00 -1430.2 8.07.6 1995.0 2.36 3.57 -.01 1911.50 -1369.2 912.3 2077.6 2.03 3.49 -.29 1912.,00 -1307.7 999.5 2131.5 2.05 2.90 -1. 25 1912.50 -1289.0 1073.7 2205.1.62 2.47 -.59 1913.00 -1349.8 1150.9 2347.5 -2.02 2.57 1.69 1913.50 -1422.0 1183.5 2459.4 -2.40 1.08.68 1914.00 -1484.8 1165.9 2544.6 -2.09 -.58 -.20 1914.50 -1555.8 1127.6 2658.4 -2.36 -1.27.74 1915.00 -1603.6 1070.8 2750."3 -1.59 -1.89.01 1915.50 -1645.8 1023,2 2846.3 -1,40 -1.58.15 1916.00 -1676.0 987,2 2948.4 -1.00 -1.19.35 1916.50 -1665.6 943.4 3016.4.34 -1,46 -.78 1917.00 -1643.3 897,9 3080.6.74 -1.51 -.90 1917.50 -1628.9 858.5 3162.4.47 -1.31 -.32 1918.,00 -1626.3 826.1 3264.5.08 -1,07.35 1918.,50 -1622,1 798.4 3369.2.14 -.92.44 1919.00 -1592.9 770.8 3457.7.97 -.-91 -.09 1919,50 -1541,4 738.7 3547,3 1.71 -1.06 -.06 1920.00 -1479.1 700.8 3646.2 2.07 -1.26.24

Double Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity x y z U V W 1945.00.0 274.3 7.6 1945.50 -45.6 190.9 95.3 -1.52.-2.77 -.12 1946.00 -133.5 121.8 185.4 -2.93 -2.30 -.04 1946.50 -263.9 74.5 280.8 -4.34 -1.57.13 1947.00 -408.8 44.7 375.9 -4.82 -.99.12 1947.50 -550.8 31.7 463.8 -4.73 -.43 -.11 1948600 -686.4 33.9 546,,8 -4.51.07 -.28 19-48.50 -819.0 46.2 630.1 -4.42.40 -.27 1949.00 -957.9 67.,8 715.9 -4,62.72 -.19 1949.50 -1105.2 100.4 801.3 -4.91 1.08 -.20 1950.,00 -1259.0, 139.3 886.2 -5.12 1.29 -.21 1950.50 -1419,.8 175.8 97 3. 8 -5.35 1.21 -.12 1951.00 -1590.1 207.6 1064.5 -5.67 1.06 -.02 1951.50 -1765.2 238.3 1160,8 -5..83 1.02.16 1952,,00 -1905.9 275.5 1255.7 -4.69 1.23.11i 1952.50 -1991.1 331.8 1348.3 -2.83 1.87.04 1953.00 -2042,7 417.2 1453,7 -1.71 2.84.46 1953.50 -2051.7 537.2 1563,0 -.29 3.99.59 1954.,00 -2005.5 688.1 1661,,2 1.53 5.02.22 1954.50 -1927.8 845,5 1742.7.2. 59 5,24 -.33 1955,00 -1837.1 987,1 1811,5 3.02 4.72 -&' 1955.50 -1754.1 1103.6 1886.9 2.76 3.88 -.53 1956.00 -1685.6 1196.2 1963,9 2.28 3.08 -.47 1956.50 -1613.8 1275.7 2021,3 2.39 2.65 -1.13 1957.00 -1570.6 1355,4 2087.3 1,43 2,65 -.,84 1957.,50 -1591.0O 1431.4 2185,7 -.67 2,53.,23 1958.00 -1648,4 1481.5 2282.0 -1,91 '1.66.16 1958.50 -1725.9 1505,8 2372,6 -2.58.81 -.02 1959.-00 -1806,6 1501.7 2463.9 -2.69 -.13 -.00 1959.50 -1861.8 1458.5 2539.8 -1,83 -1.44 -.51 1960,~00 -1896.7 1396.8 2610.1 -1,16 -2,05 -.70 1960.50 -1927.7 1343,8 2688.9 -1.03 -1.76 -.42 1961.00 -1952,1 1306.9 2782.0 -.81 -1,23.05 1961,,50 -1961.4 1276.8 2888.2 -.30 -1.00. 49 1962.00 -1951.5 1245,7 2991 -.9.33 -1,03.40 1962.,50 -2040,9 1286.0 3262.,6 -2,97 1.34 5.97 1963.00 -2121.1 1327.9 3518.1 -2.67 1.39 5.46 1963.50 -1965.0O 1233.3 3407.7 5.20 -3.15 -6.72 1964.,00 -1804.2 1146.6 3305.9 5.35 -2.89 -6,,44 1964.,50 -1757,1 1135.5 3404.4 1.56 -.37.23 1965.00 -1711.3 1128.2 3532.8 1.52 -.24 1.23

Double Theodolite Data - Shoreline Station Time, Balloon Position Wind Veloct x Y Z U V W 2030.00.0 274.3 7.6 2030.50 -122.9 218.6 94.7 -4.09 -1.85 -.14 2031.00 -259,7 171.9 183.5 -4.56 -1.55 -.08 2031.50 -422.8 149.4 275.2 -5.43 -.74.01 2032.00 -596.4 152.4 368.4 -5.78.09.05 2032.50 -764.5 172.1 462.0 -5.60.65.07 2033.00 -930.1 2-06.7 551.7 -5.52 1.15 -.05 2033.50 -1103.1 254.7 633.4 -5.76 1.59 -.32 2034.00 -1289.5 305.7 715.9 -6.21 1.70 -.29 2034.50 -1491.7 353.0 808.1 -6.74 1.57.02 2035.00 -1702.8 396.5 903.0 -7.03 1.45.11 2035.50 -1915.5 432.5 992.4 -7.08 1.19 -.06 2036.00 -2115.0 464.7 1081.5 -6.64 1.07 -.07 2036.50 -2284.6 502.3 1177.0 -5.65 1.24.13

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Veloct X Y Z U V VT 1230.00.0 1000.0.0 1230.50 94.2 167.9 91.4 3.14 -27.73 27.91 1231.00 207.3 136.1 182.8 3.76 -1.05 3.91 1231.50 272.3 87.4 274.3 2.16 -1.62 2.70 1232.00 281.2 28.5 365.7.29 0.196 1.98.1232.50 258.5 8.1 457-.2 -.75 -.68 1.-0 1 1233.00 189.7 9.2 548.6 -2.29.03 2.29 1233.50 103.9 13.1 640.0 -2.85.12 2.86 1234.00 82.5 -44.2 731.5 -.71 -1.91, 2.04 123.4.50 -26-101.4 822.9 -2.84 -1.90 3.42 1235.00 -87.9 -158.6.914.4 -2.84 -1.90 3.42 1235.50 -173.1 -215.8 1005.8 -2.84 -1.90.3.42 1236.00 -258.3 -273.1 1097.2 -2.84 -1.90 3.42 1236.50 -343.6 -330.3 1188.7 -2.84 -1.-90 3.42 1237.00 -428.8 -387.5 '1280.1 -2.84 -1.90 3.42 1237.50 -55269 -427.3 1371.6 -4.13 -1.32 4.34 1238.00 -686.5 -444.1 1463.0 -4.45 -.55 4.48 1238.50 -806.1 -486.2 1554.4 -3.98 -1.40 4.22 1239.00 -890.3 -465.4 1645.9 -2.80.69 2.89 1239.50 -940.6 -452.6 1737.3 -1.67.42 1.72 1240.00 -971.6 -444.8 1828.8 -1.03.26 1.06 1240.50 -978.3 -419.3 1920.2 -.22.85.88 1241.00 -1006.1 -376.1 2011.6 -.92 1.43 1.71 1241.50 -1083.9 -343.8 2103.1 -2.59 1.07 2.80 1242.00 -1178.1 -322.3 2194.5 -3.14.71 3.22 1242.50 -1291.1 -298.0 2286.0 -3.76.80 3.85 1243.00 -1431.6 -299.0 2377.4 -4.68 -.03 4.68 1243.50 -1555.1 -336.2 2468.8 -4.11 -1.23 4.29 1244.00 -1684-.8 -407.5 2560.3 -4.32 -2.37 4.93 1244.50 -1839.9 -438.3 2651-.7 -5.17 -1.02 5.-27.1245.00 -1974.5 -470.3 2743.2 -4.48 -1.06 4.61 1245.50 -2100.9 -562.9 2834.6 -4.21 -3.08 5.22 -1246.00 -2205.1 -691.0 2926.0 -3.47. -4.26 5.50 1246.50 -2282.7 -821.8 3 017.5 -2.58 -4.35 5.06 1247.00 -2314.2 -968.0 3-108.,9 -1.05 -4.87 4.98 1247.50 -2309.0 -1071.83200.4.17 -3.45 3.46 1248.00 -2314.3 -1184.23291.8 -..17 —,3..74.3.75 1248.50 -2301.0 -1339.233'83.2 44-5.16 5.18 1249.00 -2299.1 -1516-.03474.7...06 -.9 5.89 1249.50 -2334.5 -1690.4356'6.1 -1.17 -5.81 5.93 1250.00- x % I- - -237. -1879.43657.6 -- I 1.22 -6.9.41

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X y Z U V VT 1300.00.0.0.0 1300.50 89.0 - 93.5 91.4 2.96 -3.11 4.30 1301.00 233.2 -184.2 182.8 4.80 -.3.02 5.67 1301.50 343.4 -276.1 274.3 3.67 -3.06 4.78 1302.00 376.8 -331.0 365.7.1.11 -.1.82 2.14 1302.50 363.9 -351.4 457.2 —.42 -.68.80 1303.00 342.0 -385.2 548.6 -.73 -1.12 1.34 1303.50 266.7.-395.5 640.0 -2.50 -.34 2.53 1304.00.198.5 -399.9 731.5 2-227 -.14 2.27 1304.50 129.4 -431.5 822.9 — 2.30 -1.05 2.53 1.30-5.00 32.2 -419.3 914.4 -3.24.40 3.26 1305.50 -124.5 -431.3 1005.8 -5.22 -.40 5.24 1306.00 -28164 -443.3 1097.2 -5.22 -.40 5.24 1306.50 -438.2 -455.4 1188.7 -5.22 -.40 5.24 1307.00 -598.8 -460.4 1280.1:. -5.35 -.16 5.35 1307.50 -759.4 -465.3 1371.6 -5.35 -.16 5.35 1308.00 -852.4 -443.7 146-3.0 -3.09.72 3.18 1308.50 -995.2 -430.6 1554.-4 -4.75.43 4.77 1309.00-1034.3 -403.2 1645.9 -1.30.91 1.59 1309.50-1058.8 -377.0 1737.3 -.81.87 1.19 1310.00-1131.0 -332.9 1828.8 -2.40 1.46 2.82 1310.50-1203.3 -288.8 1920.2 -2.40 1.46 2.82 13 11.00-1316.5 -258.2 2011.6 -3.77 1.02 3.90 1311.50-1461.9 -252.5 2103.1 -4.84 19 4.85 1312.00-1608.8 -260.5 2194.5 -4.89 -.26 4.90 1312.50-1731.0 -283.4 2286.0 -4.07 -.76 4.14 1313.00-1840.7 -248.8 2377.4 -3.65 1.15 3.83 1313.50-1946.5 -259.7 2468.8 -3.52 -.36 3.54 1314.00-2038.7 -333.8 2560.3 -3.07 -2.47 3.94 1314.50-2111.7 -429.6 2651.7 -2.43 -3.19 4.01 1315.00-2140.0 -533.5 2743.2 -.94 -3.46 3.59 1315.50-=2135.4 -616.3 2834.6.15 -2.75 2.76 1316.00-2137.0 -739.9 2926.0 -.05 -4.12 4.12 1316.50-2146.9 -889.2 3017.5 -.32 -4.97 4,98 13 17.00-2186.8 -1057.1 3108.9 -1.33 -5.59 5.75 1317.50-2224.9 -1218.1 3200.4 -1.27 -5.36 5.51 1318.00-2251.8 -1390.7 3291.8 -.89 -5.75 5.82 1318.50-2238.9 -1561.9 3383.2.42 -5.70 5.72

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V VT 1500.00.0O 1000.0.0 1500.50 91.5 96.5 91.4 3.05 -30.11 30.027 1501.00 237.8 14.5 182.8 4.87 - 3.70 6.12 1501.50 330.6 -97.9 274.3 3.09 ~-:.2.77 4.15 1502.00 313.2 - 149,4 365.7 -.57-' 7 1 1.81 1502.50 262.1 - 193.9 457.2 -1.70 -1.48 2.26 1503.00 185.4 - 217.1 548.6 -2.55 -.77 2.66 1503.50 101.4 -244.9 640.0 -2.80 -.92 2.94 1504.00 2.3 - 273.4 731.5? -3.30 -.95 3.43 1504.50 - 118.8 - 301.6 822.9 -4.03-.93 4.14 1505.00 - 267.5 - 294.0 9.4.4 -4.95.25 4.96 1505.50 - 420.2 - 285.5 1005.8 -5.08.28 5.09 1506.00 - 603.2 - 266.0 1097.2 -6.10.65 6.13 1506.50 - 802.6 - 231.6.1188P7 -6.64 1.14 6.74 1507.00 -998.0 - 219.4 1280.1 -6.51.40 6.52 1507.50 - 1192.0 - 176.0 1371.6 -6.46 1.44 6.62 1508.00 - 1354.3 - 118.4 1463.0 -5.41 1.91 5.74 1508.50 - 1479.4 - 49.0 1554.4 -4.17 2.31 4.76 1509.00 - 1550.9 18.9 1645.9 -2.38 2.26 3.28 1509.50 - 1594.9 91.9 1737.3 -1.46 2.43 2.84 1510.00 - 1645.8 202.1 1828.8 -1.69 3.67 4.04 1510.50 - 1718.0 318.4 1920.2 -2.40 3.87 4.56 1511.00 - 1780.7 450.6 2011.6 -2.09 4.40 4.87 1511.50 -.1845.o7 599.7 2103.1 -~2.16 4.97 5.42 1512.00 - 1934.5 731.0 2194.5 -2.96 4.37 5.28 1512.50 - 2039.1 865.6 '2286.0 -3.48 4.48 5.68 1513.00 - 2126.9 1005.4 2377.4 -2.92 4.66 5.50 1513.50 - 2192.1 1097.7 2468.8 -2.17 3.07 3.76 1514.00 - 2267.4 1130.5 2560.3 -2.50 1.09 2.73 1514.50 -' 2359.7 1105.4 2651.7 -3.07 -.83 3.19 1515.00 - 2446.9 1038.7 2743.2 -2.90 - 2.22 3.66 1515.50 - 2476.4 950.6 2834.6 -.98 - 2.93 3.09 1516.00 - 2481.0 830.1 2926.0 -.15 - 4.01 4.01 1516.50 - 2498.1.669.4 3017.5 -.57 - 5.35 5.38 1517.00 - 2532.8 496.9 3108.9 -1.15 -5.74 5.86 1517.50 - 2560.2 337.0 3200.4 -.91- 5.32 5.40 1518.00 - 2573.2 145.9 3291.8 -.43 6.37 6.38 1518.50 - 2586.3 - 45.1 3383.2.-.43 - 6.37 6.38 1519.00 - 2569.5 - 238.3 3474.7 -.55 - 6.44 6.46 1519.50 - 2555.6 - 429.5 3566.1 -.46 - 6.37 6.38

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Ve locit X z u V VT 1530.00 ~ 0.0 0 1530.50 86.5 -175.9 91.4 2.88 -5.86 6.53 1531.00 206.5 -305.0 182.8 3.99 -4.30 5.87 1531.50 233.2 -361.9 274.3.89 -1.89 2.09 1532.00 225.4 -408.3 365.7 -.26 -1.54 1.56 1532.50 171.2 -432.5 457.2 -1.80 -.80 1.97 1533.00 107.8 -439.2 548.6 -2.11 -.22 2.12 1533050 33.4 -455.3 640.0 -2.48 -.53 2.53 1534.00 - 89.3 -441.3 731.5 -4.09.46 4.11 1534.50 - 212.1 -427.2 822.9 -4.09.46 4.11 1535.00 - 347.8 -428.0 914.4 -4.52 -.02 4.52 1535.50 - 477.6 -427.1 1005.8 -4.32.03 4.32 1536.00 - 621.8 -411.5 1097.2 -4.80.51 4.83 1536.50 - 759.7 -390.4 1188.07 -4.59.70 4.64 1537.00 - 899.6 -367.1 1280.1 -4.66.77 4.72 1537.50 - 960.4 -286.7 1371.6 -2.02 2.68 3.35 1538.00 -1021.2 -206.3 1463.0 -2.02.2.68 3.35 1538.50 -1082.0 -125.9 1554.4 -2.02 2.68 3.35 1539;.00 -1142.8 - 45.5 1645.9 -2.02 2.68 3.35 1539.50 -1203.6 34.8 1737.3 -2.02 2.68 3.35 1540.00 -1264.4 115.2 1828.8 -2.02 2.68 3.35 1540.50 -1325.1 195.7 1920.2 -2.02 2.68 3.35 1541.00 -1386.4 302.3 2011.6 -2.04 3.55 4.09 154l1-50 =1456.3 382.0 2103.1 =2.32 2.65 3.53 1542.00 -1493.0 450.7 2194.5 -1-2.2 2.28 2.59 1542.50 -1536.4 ~469.7 2286.0 -1.44..63 1.57 1543.00 =1608.5 452.1 2377.4 -2.40 -.58 2.47 1543.50 =1637.6 393.1 2368.8 -.96 -1.96 2.19 1544.00 -1629.6 296.1 2560.3..26 -3.23 3.24 1544.50 -1654.0 176.7 2651..7 -.81 =3.97 4.06 1545.00 =1673.7 46.7 2743.2 -.65 -4,33 4.38 1545.50 -1694.4 - 82.8 2834.6 -.68 -4.32 4.37 1546-.00 -1713.6 -240.8 2926.0 -.63 -5.26 5.30 1546.50 -1713.2 -386.0 3017.5.01 =4.84 4.84 1547.QO -1715.6 -527.7 3108.9 -.07 -4-72 4.72 1547-50 -1737.1 -584.5 3200.4 -.71 =1.89 2.02 1548.00 =1682.1 -816.8 3291.8 -1.83 -7.74 7.95 1548.50 =1650.9 -953.1 3383.2 1q04 -4.54 4.66 1549.00 -1565.8 -1080.2 3474.7 2.83 -4.23 5.09 1549.50 =1459.4 =l203.6 3566.1 3.54 -4.11 5.43

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V VT 1600,00.0 1000.0.0 1600-.50 86.1 60.3 91.4 2.87 -31.32 31.45 1601.00 222.6 72.3 182.8 4.54 - 4.42 6.34 1601.50 315.6 -167.8 274.3 3.10 - 3.18 4.44 1602.00 281.8 -217.0 365.7 -1.12 - 1.63 1.99 1602.50 227.1 -254.0 457.2 -1.82 - 1.23 2.20 1603.00 156.4 -266.6 548.6 -2.35 -.41 2.39 1603.50 63.6 -277.7 640.0 -3.09 -.37 3.11 1604.00 - 34.2 -283.1 731.5 -3.26 -..17 3.26 1604.50 - 156.8 -268.4 822.9 -4.08.48 4.11 1605.00 -.267.9 -262.3 914.4 -3.70.20 3.70 1605.50 - 421.4 -255.2 1005.8 -5.11.23 5.12 1606.00 576.7 -236.5 1097.02 -5.17.62 5.21 1606.50 - 713.3 -196.4 1188.7 -4.55 1.33 4.74 1607.00 - 876.7 -151.4 1280.1 -5.44 1.50. 5.64 1607.50 - 1039.8 -101.9 1371.6 -5.43 1.64 5.68 1-608-.00 - 1170.9 -53.1 1463.0 -4.36 1.62 4.66 1608.50 - 1231.9 12.9 1554.4 -2.03 2.20 2.99 1609.00 - '1268.6 93.1 1645.9 -1.22 2.67 2.94 1609.50 - 1318.8 194.7 1737.3 -1.67 3.38 3.-7 7 1610.00 - 1369.0 351.5 1828.8 -1.67 5.22 5.48 1610.50 - 1388.9 491.8 1920.2 -.66 4.67 4.72 1611.00 - 1425.8 619.9 2011.6 -1.23 4.27 4.44 1611.50 - 1482.3 735.8 2103.1 -1.88 3.86 4.29 1612.00 - 1519.3 859.6 2194..5 -1.23 4.12 4.30 1612.50 - 1578.3 967.2 2286.9 -1.96 3.58 4.09 1613.00 - 1607.0 1047.6 2377.4 -.95 2.67 2.84 1613.50 - 1639.8 1118.6 2468.8 -1.09 2.36 2.60 1614.00 -1700.5, 1160.0 2560.3 -2.02 1.38 2.45 1614.50 - 1781.7 1157.0 2651'.7 -2.70 -.09 2.70 1615.00 - 1832.3 1096,6 2743..2 -1.68 -2.01 2.62 161 5.50- 1838.0 1010.5 2834.6 -.18- 2.87 2.87 1616.00 -1856.8 865.9 2926.0 -.62 -4.82 4.86 1616.50 -1894.2 765.3 3017.5 -1.24 - 3.35 3.57 1617.00 -.19 13.&5 643.9 3108.9 -.64 - 4.04 4.09 161-7.50 - 1929.4 495,4 3200.4 -.53 - 4.95 4.98 1618.00 - 1947.8 343.4 3291.8 -.61 - 5.06 5.10 1618.50- 1951,5 194.8 3383.2 -.12 - 4.95 4095 1619.00 - 1957.1 54.6 3474.7 -.18 - 4.67 4.67

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Veloct X Y Z U V VT 1630.00.0.0.0 1630.50 96.~2 -168.7 91.4 3.20 -5.62 6.47 1631.00 229.5 -329.1 182.8 4.44 -5.34 6.95 1631.50 296.7 -411.4 274.3 2.23 -2.74 3.54 1632.00 258.8 -453.7 365.7 -1.26 -1.40 1.89 1632.50 193.7 -477.1 457.2 -2.16 -.77 2.30 1633.00 111.1 -481.3 548.6 -2.75 -.14 2.75 1633.50 30.2 -467.4 640.0 -2.69.46 2.73 1634.00 - 69.9 -457.1 731.5 -3.33.34 3,35 1634.50 -189.1 -461.1 822.9 -3.97 -.13 3.97 1635.00 -304.0 -457.6 914.4 -3.83.11 3.83 1635.50 -438.3 -436.7 1005.8 -4.47.69 4.52 1636.00 -586.0 -419.5 1097'.2' -4.92. 57 4.95 1636.50 -745.7 -409.9 1188.7 -5.32.31 5.33 1637.00 -899.4 -394.8 1280.1 -5.12.50 5.14 1637.50 -1060.7 -379.7 1371.6 -5.37.50 5.39 1638.00 -1215.1 -359.9 1463.0 -5.14.66 5.19 1638.50 -1336.9 -301.2 1554.4 -4.05 1.95 4.50 1639.00 -1403.9 -217.3 1645.9 -2.23 2.79 3.58 1639.50 -1448.5 -108.9.1737.3 -1.48 3.61 3.90 1640.00 -1491.5 - 7.7 1828.8 -1.43 3.37 3.66 1640.50 -1507.2 108.0.1920.;2 -.52 3.86 3.89 1641.00 -1537.3 232.5 2011.6 -1.00 4.14 4.26 1641.50 -1556.6 353.6 2103.1 -.64 4.03 4.09 1642.00 -1583.0 456.9.2194-.5 -.88 3.44 3.55 1642.50 -1619.8 548.3 2286.0 -1.22 3.04 3.28 1643.00 -1670.4 591.6 2377.4 -1.68 1.44 2.21 1643.50 -1748.4 615.7 2468.8 -2.59.80 2.72 1644.00 -1837.9 586.6 2560.3 -2.98 -.97 3.13 1644.50 -1862.7 544.7 2651.7 -.82 -1.39 1.62 1645.00 -1863.7 464.7 2743.2 -.03 -2.66 2.66 1645.50 -1878.7 355.0 2834.6 -.49 -3.65 3.69 1646.00 -1897.4 256.5 2926.0 -.62 -3.28 3.34 1646.50 -1901.4 153.0 3017.5 -.13 -3,45 3,45 1647.00 - 1897.3 36.4 3108.9.13 -3.88 3.88 1647.50.-1891.0 - 79.2 3200.4.21 -3.85 3.86 1648.00 -1877.7 -167.5 3291.8.44 -2.94 2.97 1648.50 -1862.6 -325.0 3383.2.50 -5-25 5.27 1649.00 -1829.8 -425.8 3474,7 1.09 -3.35 3.53 1649.50 -1770.7 -541.1 3566.1.1.97 -3.84 4.32

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V VT 1700.00.0 1000.0.0 1700.50 78.3 59.0 91.4 2.61 -31.36 3 1.47 1701.00 212.2 - 77.2 182.8 4.46 - 4.54 6.36 1701.50 248.8 -153.0 274.3 1.21 - 2.52 2.80 1702.00.201.6 -200.9 365.7 -1.57 - 1.59 2.24 1702.50 154.9 -238.6 457.2 -1.55 - 1,25 2.00 1703.00 99.9 -270.1 548.6 -1.83 - '1.04 2.11 1703.50 30.3 -288.7 640.0 -2.31.62 2.40 1704.00 -50.0 -298.8 731.5 -2.67 - 33- 2.69 1704.50 -139.8 -305.3 822.9 -~2.99 -.21 3.00 1705.00 -260.1 -298.1 914.4 -4.01 -.23 4.01 1705.5Q. - 37 41.5 -282.2 1005.8 -3.81. 53 3.85 1706-.00 -518.1 -257.2 1097.2 -4.78.83 4.85 1706.50 -657.1 -241.7 1188.6 -4.63.51 4.66 1707.00 -.803.3 -213.7 1280.1 -4.87.93 4.96 1707.50 -958.1 -179.2 1371.6 -5.15 l*15 5.28 1708.:00 -1125.6 -144.1 1463.0 -5.58 1.1-7 5.70 l.7O8,.-50 -1287.4 - 90.0 1554.4 -5.39 1.80 5.68 1709.00 17.0 1395.7 1645.9 65.90 1709.50 -1439.3 93.0 1737.3 65. 13 1710.00 -1479.3 244.7 1828.8 -1.33 4.38 4.58 1710.50 -1519.2 356.3 1920.2 -1.33 4.38 4.58 1711.00 -1587.4 518.8 2011.6 -2.27 5.41 5.87 1711.50.1.558.8 623.5 2103.1.95 3.48 3.61 1712.00 -1591.5 732.0 2194.5 -1-09 3.61 3,. 78 1712.50. -1605.7 825.2 2286.0 -.47 3.10 3.14 1713.00 -1626.1 897.6 2377.4 -.68 2.41 2.50 1713.50 -1668.4 940.1 2468.8 -1.40 1.41 1.99 1714.00 -1737.6 931.7 2560.3 -2.30 -.27 2.32 1714.50 -1767.5 900.6 2651.6 -.99 -.1.03 1.43 1715.00 -1759.5 839.2.2743.0'2.26 - 2.04 2.06 1715.50 -1769.2 762.0 2834.6 -.32 - 2.57 2.59 1716.00 -1803.2 663.7 2926.0 -1.-15' - 3.27 3.47 1716.50 -1818.2 576.8 3017.5 -.48 - 2.89 2.93 1717.00 -1816.1.496.8 3108.9.07 - 2.66 2.66 1717.50 -1803.2 403.0 3200.4.42 - 30.1-2 3.15 1718.00 -1791.1 306.1 3291.8.40 - 3.22 3.2 5 1718.50 -1770.1 220.4 3383.2.70 -, 2.85 2.94 1719.00 -1757.8 132.1 3474.7.40 - 2.94 2.97

Single Theodolite Data- Shoreline Station Time Balloon Position, Wind Veloci X Y Z U V VT 1730.00.0.0.0 1730.50 72.2 -185.2 91.4 2.40 -6.17 6.62 1731.00 196.3 -349.9 182.8 4.13 -5.49 6.87 1731.50 216.2 -400.0 27403.66 — l.66 1.79 1732.500 183.4 -419.8 365.7 -1.09 -.66 1.27 1732.50 136.0 -444.9 457.2 -1.58 -.83 1.78 1733.00 59.1 -461.5 548.6 -2.56 -.55 2.62 1733.50 - 28.6 -467.5 640.0 -2.92 -.20' 2.93 1734.00 -135.2 -473.2 731.5 - 3.55 -.18 3.55 1734.50 -241.8 -478.8 822.9 -3.55 -.18 3,55 1735.00 -360.6 -471.7.914.4 -3.95.23 3.96 1735.50 -487.3 -460.8 1005.8 -4.22.036 4.23 1736.00 -639.1 -433.6 1097.2 -5.05.90 5.13 1736.50 -790.9 -406.4 1188.7 -5.05.S90 5.13 1737.00 -956.1 -3708.8 1280.1 -5.50 1.18 5.63 1737.50 -1102.3 -330.7' 1371.6 -4.87 1.33 5.05 1738.00 -1249.4 -281.5 1463.0 -4.90 1.63 5.16 1738.50 -1402.7 -217.1 1554.4 -5.10 2.14 5.54 1739.00 -1544.6 -140.6 1645.9 -4.73 2.55 5.37 1739.50 -1558.1 - 38.7 1737.3 -.45 3.39 3.42 17.40.00 -1571.7 63.1 1828.8 -.45 3.39 3.42 1740.50 -1545.2 173.3 1920.2.88 3.67 3.77 1741.00 -15.21..2.' 292.9 2011.6.80 3.098 4.06 1741.50 -1504.5 3.97.5 2.103.4I.55 3.48 3.531 1742.00 -1487.3 468.9 2194.5 -.,57, 2.-38 2.-,4-4' 1742.50 -1507.8 519.2 2286.0O -'.68. 1.67 1.801 1.743.00 -1541.1 542.7 2377.4 -1.11.781 1.3-6 1L743.50 -1541.5 5.07 G.0 2468.8 -.-01 1. 18 11 1744.00 -1.541.8 471.4 2560.-3 -.01 1.-18. 1.18. 1744.50 -152.1.5 404.8 265.1..7.,67 2..21 2.:31 1745.00 -1516..3 330.6 2743.2.17 2.47 2.,48 1745.50 -1522.4 2.65.7 2834-.6 -.20 2-.16 2.17 1746.00 41495.9 2.0'7.5 292.6.0. 8 8 1.93 2.1 3 1746.50 -1444.0 154.3 30-17.5 1.73- 1.77 2.47 1747.00 -1394.7 8.2.8 3 108.;9 1.64 2..38 2.89' 1747.50 -1358.4 11.8 3200-.4 1,21. 2 4.,3 6 2.65 1748.00 -1,309.0O -47.9 3291.8 1.'564 1.199, 2.5-8 1748.50 -1261.3 -94.,8 3383.2 1.-59- 1. 5:6 2-.22 1749,00 -1.1.88.9 -133.3 3.474.7- 2.41, 1..28 2.73 1749.50 -1.111. 1 -198.8 3566.1 2.59 2.18 3.39 1750.00 -1026.8 -273.2 3657.6 2.80 2.47 3.74

Single Theodolite Data - Shoreline Station T ~~Balloon Position Wid, el X Y Z 13 V VT 1-800.00..0.0.0 1800.50 80.6 -178.7 91.4 2.68 -5.95 6. 53 1801.00 203.8 -318.7 182.8 4.10 -4.66 6.21 1801.50 246.0 -380.3 274.3 1.40 -2.05 2.48 1802.00 206.6 -421.9 365.7 -1.31 -1.38 1.90 1802.50 153.6 -461.9 457.2 -1.76 -1.33 2.21 1803.00 82.1 -490.6 548..61 -2.38 -.95 2.57 1803.50.0 -500.0 640.0 -2.73 -.31 2.7.5 1804.00 - 74.9 -495.2 731.5 -2.49.16 2.50 1804.50 -178.2 -484.4 822.9 -3.44.35 3.46 1805.00 =297.9 -464.1 914.4 -3.99.67 4.04 1805.50 -435.0 -453.6 1005.8 -4.56 035 4.58 1806.00 -582.3 -424.6 1097.2 -4.91.96 5.00 1806.50 -737.1 -396.1 1188.7 -5.15.095 5.24 1807.00 -891.8 -367.5 1280.1 -5.15 9 5 5.24 1807.50 -1049.1 -326,.7 1371.6 -5.24 1.36 5.41 1808.00 -1212.7 -282.1 1463.0 -5.45 1.48 5.65 1808.50 -1379.6 -235.8 1554.4 -5.56 1.54 5.77 1809.00 -1509.9 -164.0 1645.9 ~-4.34 2.39 4.95 1809.50 -1557.5 - 62.5 1737.3 -1.58 3.38 3.73 1810.00 -1544.6 48.5 1828.8B.42 3.70 3.72 1810.50 -1513.3 161.7 1920.2 1.04 3.77 3.91 1811.00 -1474.3 273.2 2011.6 1.29 3.71 30.93 1811.50 -1466.4 387.4 2103.1.26 3.80 3.81 1812.00 -1458.9 482.5 2194.5.2 5 3.16 3.17 1812.50 -1463.4 538.4 2286.0 -.15 1.86 1.87 1813.00 -1495.0 579*9 2377.4 -1.05 1.38 1.73 181-3.50 -1520.0 565.3 2468.'8 -.83 -.48.96 1814.00 -1524.4 524.9 2560.3 -.14 -1.34 1.35 1814.50 -1507.5 475.3 2651.7.56 -1.65 1.74 1815.00 =1508.5 42L5.5 2743.2 -.03 -1.99 1.99 1815.50 -1520.9 367.9 2834.6 -.41 -1.58 1.63 1816.00 -1509.0 320.7 2926.0.39 -1.57 1.62 1816.50 -1477.8 281.9 3017.6 1.04 -1.29 -1.66 1817.00 -1432.6 221.8 3108.9 l.50 — 2.00 2.50 1817.50 -1402.1 162.2 3200.4 1.01 -1.98 2.22 1818.00 -1358.3 118.8 3291.8 1.46 -1.44 2.05 1818.50 -1316.7 78.2 3383.2 1.38 -1.35 1.93 1819.0 -0 0-1263.6 50.~ 7 34d74,-7 1.-76; -.91 1.99q

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocit~y X Y Z U V VT 2015.00.0 1000.0.0 2015.50 - 73.4 181.8 91.4 -2.44 -27.27 27.38 2016.00 - 194.9 166.5 182.8 -4.05 -.51 4.08 2016.50 - 385.8 159.8 274.3 -6.36 -.22 6.36 2017.00 - 53208 129.8 365.7 -4.90 -.99 5.00 2017.50 - 711.1 131.8 457.2 -5.94.06 5.94 2018.00 - 883.-;7 143.1 548.6 -5.75.37 5.,i76 2018.50 - 1050.9 173.9 640.0 -5.57.1.02 5.66 2019.00 - 1237.3 220.4 731.5 -6.21 1.54 6.40 2019.50 - 1451.8 279.6 822.9 -7.14 1.97 7.41 2020.00 - 1637.2 330.1 914.4 -6.17 1.68 6.40 2020.50 -: 1844.6 382.0 1005.8 -6.91 1.72 7.12 2021.00 -'2072.8 429.2 1097.2 -7.60 1.57 7.76 2021.50 - 2236.0 463.0 1188.7 -5.43 1.12 5.55 2022.00 - 2364.9 502.7 1280.1 -4.29 1.32 4.49 2022.50 - 2480.0 581.7 1371.6 -3.83 2.63 4.65 2023.00 - 2475.7 662.4 1463.00.14 2.69 2.69 2023.50 - 2465.5 749.1 1554.4.33 2.88 2.90

Single Theodolite Data - Shoreline Station Time Balloon Position Wind Velocity X Y Z U V VT 2030.00.0 1000.0.0 2030.50 98.8 174.6 91.4 -3.29 -27.51 27.70 2031.00 - 248.8 164.7 182.8 -5.00 -.33 5.01 2031.50 - 424.2 142.7 274.3 -5.84 -.73 5.89 2032.00 - 595.3 148.4 365.7 -5.70.18 5.70 2032.50 - 761.0 167.3 457.2 -5.52.63 5.56 2033.00 - 913.6 199.2 548.6 -5.08 1.06 5.19 2033.50 -1116.8 253.7 640.-00 -6.77 1.81 7.01 2034.00 -1321.0 317.1 731.5 -6.80 2.11 7.12 2034.50 -1519.0 359.0 822.9 -6.59 1.39 6.'74 2035.00 -1717.4 402.8 914.4 -6.61 1.45 6.77 2035.50 -1941.7 441.J 1005.8 -7.47 1.27 7.58 2036.00 -2170.0 469.2 1097.2 -7.60.93 7.66 2036.50 -2308.3 507.5 1188.7 -4.61 1.27 4.78 2037.00 -2382.0 567.5 1280.1 -2.45 1.99 3.16 2037.50 -2398.8 647.2 1371.6 -.56 2.65 2 i.71 2038.00 -2423.8 773.5 1463.0 -.83 4.20 4.29 2038.50 -2429.5 947.2 1554.4 -.18 5.78 5.79 2039.00 -2413.2 113Q,5 1645.9.54 6.10 6.13 2039.50 -2357.8 1307.0 1737.3 1.84 5.88 6.16 2040.00 -2287.0 1418.0 1828.8 2.35 3.70 4.39 2040.50 -2210.1 1502.0 1920.2 2.56 2.80 3.79 2041.00 -2178.2 1576.8 2011.6 1.06 2.49 2.70 2041.50 -2118.3 1661.0 2 103.1 1.99 2.80 3.44 2042.00 -2083.6 1717.6 2194.5 1.15 1.88 2.21 2042.50 -2114.0 1748.9 2286.0 -1.01 1.04 1.45 2043.00 -2169.3 1775.6 2377.4 -1.84.88 2.04 2043.50 -2238.5 1812.7 2468.8 -2.30 1.23 2.61 2044.00 -2279.2 1832.6 2560.3 -1.35.66 1.50 2044.50 -2329.4 1768.1 2651.7 -1.67 - 2.14 2.72 2045.00 -2342.1 1745.8 2743.2 -.42 -.74.85 2045.50 -2329.8 1717.7 2834.6.40 -.93 1.02

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1100.00 8046.7 304.8,0 1100.50 7960.4 343.4 110.2 -2.87 1.28.62 1101.00 7892.2 380.4 203.8 -2,27 1.23.07 1101.50 7834.4 408.0 287.6 -1.92.92 -.25 1102.00 7778.9 418.7 368.3 -1.84.35 -.35 1102.50 7715.3 418.6 464.7 -2.12 -.00.16 1103.00 7628.3 409.9 591,6 -2.89 -.28 1.18 1103.50 7532.0 376.0 723.2 -3.21 -1.13 1.34 1104.00 7452.5 304.2 845.1 -2.64 -2.39 1.01 1104.50 7387.8 214.3 971.9 -2.15 -2.99 1.17 1105.00 7342.1 139.4 1094.4 -1.52 -2.49 1.03 1105.50 7327.8 89.0 1187.1 -.47 -1.67.04 1106.00 7324.7 50.4 1243.0 -.10 -1.28 -1,018 1106.50 7307.1 8.0 1289.9 -.58 -1.41 -1.48 1107.00 7256.2 -39.3 1366.3 -1.39 -1.57 -.50 1107.50 7196.7 -81.9 1486.9 -2.28 -1.42.97 1108.00 7121.7 -106.7 1623.0 -2.50 -.82 1.48 1108.50 7070.3 -109.0 1709.6 -1.71 -.07 -.16 1109.00 7038.9 -114.9 1737.7 -1.04 -.19 -2.11 1109.50 6990.3 -149.2 1766.7 -1.61 -1.14 -2.08 1110.00 6903.8 -202.6 1826.2 -2.88 -1.77 -1.06 1110.50 6803.8 -259.9 1891.4 -3.33 -1.90 -.87 1111.00 6706.2 -325.9 1953.1 -3.25 -2,20 -.99 1111.50 6609.8 -409.0 2016.9 -3.21 -2.76 -.91 1112.00 6450.6 -551.1 2183.8 -5.30 -4.73 2.51 1112.50 6236.7 -745.4 2436.4 -7.12 -6.47 5.37 1113.00 6112.9 -896.2 2547.0 -4.12 -5.02.63 1113.50 6109.0 -987.8 2504.3 -.12 -3.05 -4.47 1114.00 6173.9 -1064.4 2424.8 2.16 -2.55 -5.69 1114.50 6238.1 -1163.2 2381.6 2.14 -3.29 -4.48 1115.00 6265.7 -1290.1 2404.8.91 -4.23 -2.27 1115.50 6302.5 -1396.4 2428.7 1.22 -3.54 -2.25 1116.00 6308.3 -1515.8 2483.7.19 -3.97 -1.21 1116.50 6260.7 -1690.3 2599.2 -1.58 -5.81.80 1117.00 6274.9 -1819.1 2632.0.47 -4.29 -1.95 1117.50 6321.0 -1926.8 2623.4 1.53 -3.58 -3.33 1118.00 6334.7 -2073.5 2663.7.45 -4.89 -1.70 1118.50 6392.6 -2160.3 2642.2 1.93 -2.89 -3.76 1119.00 6469.3 -2244.3 2615.7 2.55 -2.80 -3.93 1119.50 6506.4 -2434.3 2699.8 1.23 -6.33 -.24 1120.00 6531.1 -2674.6 2840.9.82 -8.01 1.65

Double Theodolite Data - 8 K-M Station Time Balloon Posit~ion Wind Velocit~y x y z U V W 1130.00 8046.7 304.8.0 1130.50 7991.8 319.4 182.9 -1.83.48 3.05 1131.00 7942.4 328.9 368.5 -1,64.31 3.13 1131.50 7903.9 328.b3 559.3 -1.28 -.02 3.31 1132.00 7870.8 322.5 752.,8 -1.10 -.19 3.40 1132.50 7838.2 314.1 947.3 -1.08 -.28 3.43 1133.00 7807.9 303.7 1142.5 -1,01 -.34 3.45 1133.50 7778.,3 287. 3 1311.1 -.98 -.54 2.56 1134.,00 7749.1 258.7 1433.6 -.97 -.95 1.03 1134.50 7726.4 235.2 1536.1 -.75 -.78.36 1135.00 7707.2 233.0 164-2.4 -.64 -.07.49 1135.50 7671.0 243.1 1755.5 -1.20.33.72 1136.00 7603.2 244.9 1857'.'7'.- -2.26.05.35 1136.50 7517,2 229.3 1934.0 -2.86 -.51 -.50 1137.,00 7422.0 201.0O 2003.1 -3.17 -.*94 -.74 1137.50 7308.5 161.3 2071.1 -3.78 -1.32 -.78 1138.00 7165.7 100.7 2158.0 -4.76 -2.01 -.15 1138.50 7034.,8 22.3 2235.2 -4.36 -2.61 -.47 1139.00 6934.8 -70.3 2292.,2 -3.33 -3.08 -1.14 1139.50 6812.5 -179.9 2400.4 -4.07 -3.65.55 1140.,00 6675.3 -296.0 2523.5 -4/.-5 7 -3.87 1.05 1140.50 6566.8 -415.1 2606,9 -3.61 -3097 -.,26 1141.00 6536.8 -525.8 2602.5 -1.00 -3.68 -3.19 1141.50 6555,.6 -637.1 2555.0.62 -3.70 -4.63 1142.00 6547.0 -773.8 2580.1 -.28 -4.55 -2,21 1142.50 6512.1 -925.5 2670.7 -1.16 -5,05 -.02 1143,00 6496.2 -1043,2 2725.2 -.53 -3,92 -1.23 1143.,50 6527.1 -1121.8 2698.1 1.03 -2..62 -3.95 1144.00 6533.1 -1245.8 2722.3.20 -4.13 -2.,23 1144.50 6449.1l -1475,7 2897.8 -2.79 -7.66 2.80 1145.00 6355.1 -1737.5 3086.0 -3.13 -8.72 3.22 1145. 50 6349.,4 -1925.1 3138.6 -.18 -6.25 -1.29 1146.00 6373.6 -2111.7 3.188.8.80 -6.21 -1.37 1146.50 6390.6 -2333.4 3303,0.56 -7.39.75 1147.00 6478.4 -2459.7 3312.3 2.92 -4.20 -2.73 1147.50 6608.1 -2541.3 3262.9 4.32 -2.71 -4.69 1148,00 6691.3 -2739.8 3335,2 2.77 -6.61 -.63 1148.50 6777.3 -2933,2 3403.0 2.86 -6,44 -.78 1149.~00 6903.6 -3046.1 3389.3 4.,21 -3.76 -3.50 1149.50 7007.3 -3232.5 3453.6 3.45. -6.21 -.90 1150.00 7093.0 -3462.7 3563,9 2.,85 -7.67.62

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1200.,00 8046 o 7 304.8.0 1200.50 7983.7 277.5 197.3 -2.09 -.90 3$d53 1201.00 7920.8 250.2 394.7 -2.09 -.90 3.53 1201.50 7857.8 222.9 592.1 -2.09 -.90 3.53 1202.00 7794.9 195.6 789.4 -2.09 -.90 3.53 1202. 50 7731.9 168.3 986.8 -2.09 -.90 3.53 1203.00 7669.0 141.0 1184.2 -2.09 -.90 3.53 1203.50 7611.1 136.0 1364.8 -1.93 -.16 2.97 1204.00 7560.3 160.9 1497.5 -1.69.83 1.37 1204.o50 7519.7 176.0 1575.6 -1.35.50 -.44 1205.00 7488.2 177.0 1648.8 -1.05 r.03 -.60 1205o50 7451.3 196.8 1745.3 -1.22.65.16 1206o00 7396.4 232.0 1835.7 -1.82 1.17 -.03 1206 50 7321.1 258.5 1902.5 -2.50.88 -.82 1207o00 7233.3 275~8 1954.4 -2.92.57 -1.31 1207.50 7121.8 282.7 2035.4 -3.71.22 -34 1208o00 6997.0 262.2 2117.4 -4.15 -.68 -.31 1208.o50 6873.4 208.2 2182.2 -4.12 -1.79 -.88 1209.00 6734.4 131.9 2285.9 -4.63 -2.54.40 1209.50 6608.9 48.8 2382.5 -4118 -2.77.17 1210.00 6518.2 -40.1 2441.3 -3.02 -2.96 -1.09 1210o50 6439.2 -134.2 2494~6 -2.63 -3.13 -1.26 1211o00 6379.0 -232.7 2537.5 -2.00 -3.28 -1.61 1211.50 6330.7 -354,5 2611.2 -1.61 -4.05 -.59 1212o00 6184.6 4534.0 2877~3 -4.87 -5.98 5.82 1212.50 6037~0 -719.3 3165.3 -4.91 -6.17 6.55 1213.00 6091.1 -837.7 3165,1 1.80 -3.94 -3.05 1213.50 6224.7 -930.8 3029.7 4.45 -3.10 -7.56 1214,o00 6248o1 -1087.4 3020.2.78 -5.22 -3.36 1214,50 6156o4 -1341.9 3199.7 -3.05 -8.48 2.93 1215o00 6086.3 -1604.5 3397.8 -2.33 -8.75 3.55 1215o50 6089~0 -1832.3 3536.0.09 -7.59 1.55 1216000 6151.5 -2016.2 3617.5 2.08 -6.13 -.32 1216.50 6308~4 -2102.9 3542.2 5.22 -2.88 -5.55 1217o00 6424~6 -2274.4 3560.5 3.87 -5.71 -2.43 1217o50 6527.7 -2433o1 3587.1 3.43 -5.29 -2.16 1218.00 6736.7 -2401.4 3385.8 6.96 1.05 -9 o 75 1218.50 6877.0 -2514.6 3372.1 4.67 -3.77 -3.50 1219,00 6862.3 -3120.2 3931.8 -.48 -20.18 15.60 1219.50 6820.0 -4069.0 4847.9 -1.41 -31.62 27.48 1220,00 6929~4 -4711,9 5387.8 3.64 -21.42 14.94

Double Theodolite Data - 8:K d-S-ation Time Balloon Position Wind Velocit x z U V W 1330.00 8046.7 304.8.0 1330.50 7982,.1 349.0 81.0O -2.15 1.47 -.34 1331.00 7909.8 393.1 161.0 -2.,41 1.46' -.37 1331.50 7825.8 432.0O 237.7 -2.79 1.29 -.,49 1332.00 7738.6 466.9 313.1 -2.90 1,16 -.53 1332.50 7650.3 509.9 398.3 -~2.94 1.43 -.20 1333.00 7569.8 553.8 504.0 -2.68 1.46.47 1333.50 7506.3 584.3 629.0 -2.11 1.01 1.11 1334.00 7446.3 602.2 766.2 -2.00.59 1,52 1334.50 7379.2 598.3 929.3 -2.23 -.13 2.,30 1335,.00 7325.2 566.8 1123.0 -1.79 -1.04 3.40 1335.,50 7298.4 517.2 1302.2 -.89 -1.65 2.,92 1336.00 7272.8 461.4 1427.0O -.85 -1.85 1.11 1336.50 7239.0O 408.8 1507.0 -1.12 -1,75 -.38 1337.00 7209.4 35 511 1560.8 -.98 -1.78 -1,,25 1337.50 7161.6 298,3 1615.2 -1.59 -1,,89 -1.,23 1338.00 7087.6 2321689.9 -2.46 -1.16 -.,55 1338.'50 7021.0 268.4 1759.4 -2.21.17 -.73 1339.00 6966.9 292.5 1815.2 -1.80.80 -1.,18 1339,50 6894.,8 321.2 1882.3 -2,40 095 -.81 1340,00 6794.2 356.7 1961.4 -3.35 1,,18 -.40 1340,50 6682.2 386,2 2038.9 -3.73.98 -.,46 1341.00 6565,2 400.4 2114.9 - 3.89 47-.,51 1341.50 6437.4 406.1l 2 2 127,02 -4,26.18.19 1342.,00 6317.,8 416,,6 2334,,2 -3.98.34 1.01 1342,,50 6177.1 432.2 2519.4 -4.68.52 3.12 1343,00 5990.3 416.2 2769.8 -6.22 -.53 5.29 1343.50 5850.9 345.2 2960.7 -4.64 -2.36 3.,31 1344.,00 5810.0 247.6 3070.9 -1,36 -3.26.62 1344.50 5847.7 145,0 3133,5 1,25 -3.,42 -0O, 96 1345.00 6193.3 81.9 2737.7 11.,52 -2.,10 -16,23 1345,,50 6475.8 -23,7 2404.4 9.,41 -3.,52 -14,15 1346.,00 6146.9 -275,3 2972.4 -10.,96 -8,,38 15.88 1346.,50 5926.6 -497.9 3364.3 -7,.34 -7,41 10.01 1347.00 6008.7 -682,4 3315.8 2,73 -6,15 -4.,66 1347.50 5926.1 -958.5 3566.9 -2.75 -9.20 5.32 1348.,00 5860.2 -1225.3 3829.9 -2,,19 -8.89 5.72 1348.50 5918.6 -1432,0O 3917.7 1,94 -6.88 -.12 1349.,00 6027.7 -.1601.2 3928.9 3.63 -5.64 -2.67 1349.,50 6176,8 — 1719.6 3880.5 4.,96 -3,94 -4.66 1350.00 6336.5 -1818.2 3839.7 5.32 -3.28 -4.40

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1400.00 8046.7.0.0 1400.50 7964.5 285.5 123.4 -2.73 9.51 1.06 1401,00 7892.5 420.5 233.9 -2.39 4.49.63 1401 o 50 7833 o 3 486.2 339. 1 -1.97 2.18.45 1402.00 7791.0 558.9 440.4 -1.41 2.42.32 1402.50 7759.1 623.3 534.8 -1.06 2.14.09 1403.00 7728.8 671.1 636.6 -1.01 1.59.34 1403.50 7701.7 712.0 747.6 -.90 1.36.65 1404.00 7677.9 749.4 861.7 -.79 1.24.75 1404o.50 7650.3 780.8 989.9 -.92 1.04 1.22 1405 o00 7613. 9 810 o.0 1142.1 -1.21.97 2.02 1405.50 7544.3 861.0 1353.4 -2.32 1.69 3.99 1406.00 7442.7 915,0 1556.9 -3.38 1.80 3.73 1406.50 7356.8 910.9 1641.7 -2.86 -.13 -.22 1407.00 7289.1 867.1 1686.8 -2.25 -1.46 -1.54 1407o50 7210.0 832.7 1783.0 -2.63 -1.14.15 1408.00 7107.8 830.0 1909.4 -3.40 -.08 1.16 1408.50 6994.4 858.8 2016.9 -3.77.95.53 1409.00 6882.4 896.8 2101.4 -3.73 1.26 -.23 1409.o50 6770.4 934.7 2185.9 -3.73 1.26 -.23 1410,00 6658.5 972o7 2270.3 -3.73 1.26 -.28 1410o50 6546.5 1010.6 2354.8 -3.73 1.26 -.23 1411.00 6440.5 1055.5 2464.7 -3.53 1.49.61 1411.50 6376.6 1101.1 2575.0 -2.12 1.51.62 1412.o00 6367.5 1126.5 2629.3 -.30.84 -1.23 1412 o 50 6329.5 1133.2 2712.7 -1.26.22 -.26 1413.00 6223.5 1110 1 2875.3 -3.53 -. 76 2.37 1413.50 6131.9 1039.1 3019.2 -3.05 -2.36 1.74 1414.00 6126.5 929,7 3075.3 -.17 -3.64 -1.18 1414.o50 6173o5 790.4 3086.4 1.56 -4.64 -2.67 1415o00 6203~9 622.2 3109.9 1.01 -5.60 -2.26 1415o50 6200.7 431.4 3154.0 -.10 -6.35 -1.57 1416.00 6174.3 233.3 2340.6 -.87 -6.60 -.16 1416.50 6186.5 36.1 3292.6.40 -6.57 -1.31 1417.00 6228.3 -163.3 3323.1 1.39 -6.65 -2.02 1417. 50 6245.6 -363.9 34830.2.57 -6.68.52 1418o00 6290.6 -552.9 3516.3 1.49 -6.29 -.17

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z 1430.00 8046.7 304.8.0 1430.50 7937.4 307.0 58.2 -3.64.07 -1.10 1431.00 7828.1 309.3 116.5 -3.64.07 -1.10 1431050 7716.3 315.0 176.0 -3.72.18 -1.06 1432000 7600.2 332.3 242.4 -3.86.57 -.83 1432050 7482.8 364.0 317.5 -3.91 1.05 -.54 1433.00 7366.2 406.9 397.8 -3.88 1.43 -.37 1433.50 7254.2 457.6 478.1 -3.73 1.68 -.36 1434.00 7149.2 509.0 549.6 -3.49 1.71 -o.66 1434.50 7047.2 558.6 614.6 -3.39 1.65 -.88 1435.00 6945.2 608.3 679.6 -3.39 1.65 -.88 1435,50 6856 o 3 655.8 739.8 -2,96 1.o 58 -1.o 03 1436.00 6787.4 705.0 795.2 -2.29 1.63 -1.20 1436.50 6717.1 765.4 857.3 -2.34 2.01 -.97 1437000 6625.7 831,8 932.8 -3.04 2. 21 -.53 1437.50 6517.8 891.3 1021.8 -3.59 1.98 -.08 1438.00 6409.2 948.0 1117.9 -3.61 1.89 o15 1438.50 6314.0 1001.1 1202.6 -3.17 1.77 -.22 1439,00 6236.4 1038.4 1279,2 -2.58 1.24 -.49 1439,50 6162.1 1066.o7 1367.8 -2.47 o.94 -.o09 1440.00 6084.1 1096.8 1466.5 -2 o.60 1.00 o 24 1440 50 6010,7 1133o.1 1574.8 -2.44 1.20.56 1441,00 5945.4 1172.2 1693.5 -2.17 1.30.90 1441,50 5892.4 1210.0 1807.5 -1.76 1.26.75 1442.00 5849.0 1269.7 1915.5 -1.44 1.99.55 1442.50 5831.c2 1354.9 1999.7 -.59 2.83 -.24 1443o00 5816o.9 1453.5 2067.4 -.47 3.28 -o78 1443~50 5757.8 1571.3 2165.0 -1.97 3.92.20 1444,00 5667~5 1700.8 2287.7 -3.00 4.31 1,04 1444 50 5569.3 1820.2 2403., 0 -3.27 3.98.79 1445o00 5493.2 1907.9 2469.7 -2.53 2.92 -.82 1445.50 5427.2 1976.7 2512.2 -2.20 2,29 -1.62 1446,00 5352.7 2034.2 2583.3 -2.48 1.91 -.67 1446o50 5264o1 2070.8 2697.5 -2,95 1.22.75 1447.00 513405 2094.8 2860.7 -4.32.80 2~39

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1500.00 8046.7 304.8 1500.50 7914.2 328.2 122.4 -4.41.78 1.03 1501.00 7808.3 362.0 239.5 -3.52 1.12.85 1501.50 7723.4 418.1 356.2 -2.83 1.86.84 1502.00 7652.7 482.3 479.0 -2.35 2.14 1.04 1502.50 7594.4 522.8 602.1 -1.94 1.35 1.05 1503.00 7529.2 538.3 734.6 -2' 17.51 1. 36 1503.50 7453.6 540.5 883.8 -2.51.07 1.92 1504.00 7388.6 525.8 1027.3 -2.16 -.49 1.73 1504.50 7342.4 502.4 1150.2 -1.54 -.78 1.04 1505.00 7315.6 485.9 1247.9 -.89 -.54.20 1505.50 7300.7 467.6 1332.4 -.49 -.60 -.23 1506,00 7274.9 435.2 1420.9 -.86 -1.08 -.09 1506,50 7227.7 429.8 1505.8 -1.57 -.18 -.21 1507.00 7173.4 486.3 1580.2 -1.81 1.88 -.56 1507.50 7121.1 571.0 1650.3 -1.74 2.82 -.70 1508.00 7068.9;655.7 1720.5 -1.74 2.82 -.70 1508.50 7016.6 740.5 1790.6 -1.74 2.82 -.70 1509.00 6964.4 825.2 1860.8 -1.74 2.82 -.70 1509.50 6912.1 909.9 1930.9 -1.74 2.82 -.70 1510.00 6859.9 994.6 2001.1 -1.74 2.82 -.70 1510o50 6807.6 1079.3 2071.2 -1.74 2.82 -.70 1511.00 6741.3 1155.1 2162.7 -2.21 2.52.00 1511,50 6647.8 1192.9 2291.6 -3.11 1.25 1.24 1512.00 6568.1 1163.4 2403.9 -2.65 -.98.69 1512.50 6549.2 1077.4 2466.3 -.63 -2.86 -.96 1513.00 6563.4 964.5 2527.5.47 -3.76 1513,50 6565.0 828.2 2606.8 e.05 -4.54 -.40 1514,00 6549.9 2671o4 2690.5 -.50 -5.22 -.25 1514.50 6539.2 503.4 2764.0 -.35 -5.59 -.59 1515.00 6546.4 324.9 2815.6.24 -5.95 -1.32 1515,50 6558.4 147.9 2874.8.40 -5.89 -1.07 1516,00 6575.8 -.17.2 2942.9.58 -5.50 -.78 1516,50 6611.5 -175.4 2997.9 1.19 -5.27 -1.21 1517.00 6641.4 -336.7 3089.7.99 -5.37.01 1517.50 6665.4 -503.5 3226.9.80 -5.55 1,52 1518,00 6725.1 -664,8 3343.5 1.98 -5,37.83 1518.50 6817.3 -822.8 3447.5 3.07 -5.26 o41 1519,00 6942.4 -961.5 3501.9 4.16 -4.62 -1.23 1519,50 7125.8 -1025.4 3374.8 6.11 -2.12 -7.28 1520.00 7346.2 -1010.2 3086.3 7.34.50 -12.66

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1530,00 8046,7 1530.50 8088.4 19905 124.6 1.38 6.65 1.10 1531.00 8092.1 273.1 247.7.12 2.45 1.05 1531.50 8047.5 295.6 326.5 -1.48.74 -o42 1532.00 7988.2 319.1 387.2 -1.97.78 -1.02 1532.50 7928.8 340.4 476.2 -1.98.71 -.08 1533.00 7848.6 380.5 595.3 -2.67 1.33.92 1533.50 7741.0 433.6 724.6 -3.58 1.77 1o26 1534.00 7609.9 476.2 843.6 -4.36 1.41.91 1534.50 7461.3 503.8 957.1 -4.95.91 o 73 1535.00 7311.7 524.0 1059.1 -4.98.67.35 1535.50 7171.5 540.9 1133.7 -4.67.56 -.56 1536.00 7036,8 545.7 1183.6 -4.48. 16 -1.38 1536.50 6911.8 528.8 1215.1 -4.16 -.56 -1.99 1537.00 6808.8 494.4 1242.1 -3.43 -1.14 -2,14 1537.50 6706.4 440.7 1289.0 -3.41 -1.79 -1.48 1538,00 6563.3 388.4 1389.3 -4.76 -1.74.29 1538.50 6430.2 388.3 1509.-4 -4.43 -.00.95 1539.00 6373.4 447.6 1577.3 -1.89 1.97 -.78 1539.50 6324.1 543,3 1630.2 -1.64 3.18 -1.28 1540.00 6255,1 657.3 1704.5 -2.29 3.80 -.57 1540 o 50 6217,0 770,3 1767.0 -1. 27 3.76 -.96 1541o00 6217.6 863.3 1795.6.02 3.10 -2.09 1541.50 6243.8 935.3 1795,1.87 2.39 -3,06 1542.00 6248.4 1002.0 1808.3.15 2.22 -2.60 1542.50 6220.3 1061.2 1844,8 -.93 1.97 -1.82 %543,00 6155.6 1116,4 1911,0 -2.15 1.84 -.84 1543,50 6039.2 1168.9 2023.3 -3.87 1.75.69 1544,00 5977,8 1167.5 2086.3 -2.04 -o 04 -94 1544o50 5984,8 1113.0 2107.1.23 -1.81 -2,35 1545000 5919,9 1081.6 2236.4 -2.16 -1.04 1.26

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity 1600.00 8046.7 304.8.0 1600.50 8196. 7 224.4 85.4 4.99 -2.67 -.19 1601.00 8319.8 157.1 178.1 4.10 -2.24.04 1601.50 8390.7 108.2 275.0 2.36 -1.62.18 1602,00 8409.8 62.7 373.8.63 -1.51.24 1602.50 8401.9 13.6 472.8 -.26 -1.63.25 1603.00 8392.2 -32.7 561.7 -.32 -1.54 -.08 1603.50 8399.1 -64.3 643.5.23 -1.05 -.32 1604.00 8414.0 -74.4 740.2.49 -.33.17 1604.50 8418.4 -77.9 859.7.14 -.11.93 1605.00 8405.0 -67.5 984.0 -.44.34 1.09 1605.50 8341.3 -29.0 1101.6 -2.12 1.28.87 1606.00 8219.9 12.8 1231.6 -4.04 1.39 1.28

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity 1630 00 8046.7 304. 8.0 1630650 8142.1 ~ 242.9 130.8 3.18 -2.06 1.31 1631.00 8191.1 187o4 242.5 1.63 -1.84.67 1631.50 821760 135.1 344.6.86 -1.74.35 1632.00 8223.4 87.8 440.4.21 -1.57.14 1632.50 8172,5 55.1 529.9 -1.69 -1.09 -.06 1633,00 8065.2 36.7 625 o 5 -3.57 -.61.13 1633.50 7939.5 23.1 727.3 -4.19 -.45.34 1634o00 7813.8 9.5 829.2 -4.19 -.45.34 1634.50 7688.1 -4.1 931.1 -4.19 -.45.34 1635.00 7562.4 -17.7 1032.9 -4.19 -.45.34 1635.50 7443.8 -29.5 1115.6 -3.95 -.39 -.29 1636.00 7332.1 -37,6 1172.6 -3.72 -.27 -1.14 1636.50 721104 -42.2 1239.1 -4.02 -.- 15 -.82 1637.00 7080,6 -38.9 1323.3 -4.35.10 -.24 1637.50 6956.1 -19.7 1402.2 -4.14.64 -.41 1638.00 68,57.6 25.5 1467.5 -3.28 1.50 -.87 1638.50 6785.5 101.8 1545.0 -2.40 2.54 -.46 1639o00 6717.4 198.1 1662.3 -2.27 3.21.86 1639.50 6669.9 301.9 1767.7 -1.58 3.45.46 1640. 00 6647.9 410.6 1838,9 -. 73 3.62 -.67 1640.50 6612.4 523.1 1929.8 -1,18 3.75 -.01 1641.00 6596.5 625.7 2009.9 -.53 3.41 -.37 1641,50 6609.4 703,7 2062.9.43 2.59 -1.28 1642,00 659705 758.6 2131.6 -.39 1.83 -.75 1642.50 6577.1 779.4 2185.2 -.68.69 -1.26 1643.00 6561.0 756.6 2221.5 -.53 -.75 -1.83 1643.50 6537.4 706.8 2290.2 -.78 -1.66 -.75 1644000 6521,5 636.0 2382.9 -.53 -2.36.04 1644.50 6517.3 541.2 2454.7 -.13 -3.15 -.65 1645.00 6519.3 432.8 2486.8.06 -3.61 -1.98

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1700.00 8046.7 304.8 0 1700.50 8174.5 222.5 92.6 4.26 -2.74.04 1701000 8267.7 145.5 189.5 3.10 -2.56.18 1701.50 8296.0 78.9 292.3.94 -2.22.37 1702.00 8275.0 27.3 399.7 -.69 -1.71.53 1702.50 8235.0 -7.5 507.8 -1.33 -1.16.55 1703.00 8178.4 -34.0 611.1 -1.88 -.88.39 1703.50 8098.8 -51.0 693.7 -2.65 -.56 -.29 1704.00 7997.6 -53.3 i7758.6 -3.37 -.07 -.88 1704.50 7881.3 -52.3 828.8 -3.87.03 -. 70 1705.00 7758.9 -55.6 901.5 -4.08 -.11 -.62 1705 50 7632.9 -58.7 971.7 -4.19 —.10 -.70 1706.00 7503.4 -56.7 1053.5 -4.31.06 -. 32 1706.50 7379.2 -47.3 1152.1 -4.13.31.23 1707.00 7256.9 -25.9 1250.5 -4.07.71.23 1707 50 7120.7 6.4 1341.9 -4.54 1.07 -.00 1708.00 6991.6 44.1 1424.6 -4.30 1.25 -. 29 1708,50 6888.5 89.4 1502.3 -3.43 1.51 -.46 1709.00 6792.9 156.9 1606.8 -3.18 2.24.43 1709.50 6728.6 257.5 1724.7 -2.14 3.35.87 1710.00 6715.2 376.7 1814.8 -.44 3.97 -.04 1710.50 6709.0 493.6 1893.5 -.20 3.89 -.42 1711.00 6700.5 595.0 1972.6 -.28 3.37 -.40 1711.50 6706.7 668.6 2037.9.20 2.45 -.87 1712.00 6704.1 707.2 2101.0 -.08 1.28 -.94 1712.50 6679.6 706.0 2173.6 -.81 -.03 -.62 1713.00 6663.8 666.0 2241.2 -.52 -1.33 -.79 1713.50 6660.7 601.4 2327.1 -.10 -2.15 -.18 1714,00 6659.4 523.8 2416.8 -.04 -2.58 -.05 1714.50 6656.4 436.2 2488.0 -.09 -2.91 -.67 1715.00 6624.2 346.3 2614.5 -1.07 -2.99 1.16

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1800.00 8046. 7 304.8 1800o50 8116o4 215o1 107.2 [.2.32 -2.98.52 1801o00 8157.8 12401 206.1 1.38 -3.03.24 21801.50 8171.4 38.6 301.6.45 -2.85.13 1802. 00 8152.3 -30.8 398.1 -.63 -2.31.16 1802 o50 8099.3 -83.2 497.1 -1.76 -1.74.25 1803000 8022.8 -113.8 594.8 -2.55 -1.02.20 1803.50 7937.3 -121.1 687.5 -2.84 -.24.04 1804o00 7853.3 -119.2 773.1 -2.79.06 -.19 1804 o 50 7773.2 -117 2 846,5 -2'.66.06 -.60 1805.00 7678.8 -120.6 924.9 -3.14 -.11 -.43 1805o 50 7559.2 -117.0 1008.7 -3.98.12 -.25 1806 00 7433.2 -86.4. 1084.4 -4.20 1.02 -o52 1806 o50 7308.5 -41" 5 1164.9 -4.15 1.49 -.36 1807o00 7189.3 -.9 1250.7 -3.97 1.35 -.18 1807o50 7076.6 35.8 1330.9 -3.75 1.22 -.37 1808,00 6962.1 76.7 1408.3 -3.81 1.36 -.46 1808.50 6848.8 129.8 149;3.4 -3.77 1.77 -. 20 1809.00 6745o8 206.6 1603.5 -3.43 2.56.62 1809,50 6687.2 303,7 1726.1 -1.95 3.23 1.03 18100 o 0 6701.0 406.5 1811.3.45 3.42 -.2 0 1810,50 6738.6 509.0 1866.7 1.25 3.41 -1.20 1811,00 6-750.8 597.6 1940.8.40 2.95 -.57 1811,50 6743o6 653.3 2027.3 -.23 1.85 -.16 1812,00 6721.3 675.3 2107.2 -.74.73 -.38 1812050 6711.2 665.4 2144.5 -.33 -.33 -1.80 1813,00 6722.0 629.6 2152.0.35 -1.19 -2,79 1813.50 6730.7 586.1 2201.5.29 -1.44 -1.39 1814,00 6741.3 543.8 2290.7.35 -1.41 -o07 1814050 6756.0 503.9 2372.7.49 -1.32 -o31 1815,00 6800.0 459.5 2384.1 1,46 -1.48 -2.66

Double Theodolite Data -- 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 1830.00 8046.7 304.8. 0 1830.50 8127.9 228.1 88.1 2.70 -2.55 -.10 1831.00 8190.8 153.1 167.9 2.09 -2.49 -.38 1831.50 8204.3 88.4 242.0.44 -2.15 -.57 1832.00 8173.6 36.3 314.5 -1.02 -1.73 -.62 1832o50 8121.9 -9.7 387.3 -1.72 -1.53 -.62 1833.00 8054.0 -43.2 459.5 -2.26 -1.11 -.64 1833.50 7977.2 -55,7 529.6 -2.55 -.41 -.71 1834o00 7898.4 -58.7 601.2 -2.62 -.10 -.66 1834.50 7817.1 -64 o2 674.7 -2.70 -.18 —. 59 1835.00 7732.6 -75.1 745.3 -2.81 -.36 -.69 1835.50 7642.3 -87.0 812.2 -3.01 -.39 -.81 1836.00 7547.6 -89.1 879.3 -3.15 -.07 -.81 1836.50 7449.4 -77.3 949.7 -3.27.39 -.69 1837.00 7344.1 -53.8 1021.5 -3.51.78 -.65 1837. 50 7234.4 -24.0 1086.6 -3.65..99 -.88 183800 7124.9 10.6 1139.8 -3.65 1.15 -1.27 1838.50 7015.0 49.0 1186.0 -3.66 1.27 -1.50 1839,00 6903.7 82.2 1231.7 -3.71 1.10 -1.52 1839. 50 6780.7 108.4 1289.6 -4.09.87 -1.11 1840O00 6649.4 137.7 1353.5 -4.37.97 -.91 1840.50 6527.0 175.1 1411.9 -4.07 1.24 -1.10 1841o00 6406.5 218.5 1484 3 -4.01 1.44 -.63

Double Theodolite Data - 8 KM Station Time Balloon Position Wind Velocity X Y Z U V W 19000 o 0 8046.7 304.8. 0 1900050 8081.4 266.4 95.8 1.15 -1.27.14 1901.00 8047.3 255.3 183.4 -1.13 -.37 -.12 1901.50 7978.7 257.7 266.8 -2.28.08 -.26 1902.00 7910.2 260.1 350.2 -2.28.08 -.26 1902050 7841.6 262.5 433.6 -2.28.08 -.26 1903.00 7773.0 264.9 517.0 -2.28.08 -.26 1903.50 7704.5 267,.3 600.4 -2.28.08 -.26 1904.00 7635.9 269.7; 683.7 -2.28.08 -.26 1904.50 7567.4 272.1 767.1 -2.28.08 -.26 1905.00 7498.8 274.5 850.5 -2.28.08 -.26 1905.60 7430.3 276.9 933.9 -2.28.08 -.26 1906000 7345,9 286.8 1015.0 -2.81.32 -.34 1906.50 7234.7 310.7 1087.5 -3.70.7"9 -.63 1907.00 7118.4 341.1 1150.9 -3.87 1.01 -093 1907.50 7026.3 367.4 1191.7 -3,07.87 -1,68 1908,00 6933.9 389.5 1237 9 -3,07.73 -1-50 1908.50 6806,6 425.4 1349.3 -4.24 1.19.66 1909.00 6718.3 494.3 1480.9 -2.94 2.29 1.33 1909.50 6720.4 590.2 1579.5.06 3.19.23 1910.00 679201 684.9 1634.7 2.39 3.15 -1.20 1910.50 6905.6 760.5 1650.3 3.78 2.51 -2.53 1911.00 6994.6 831.3 1685.7 2.96 2.36 -1.86 1911.50 7039.2 912.4 1761o 7 1.48 2.70 -o 51 1912000 7072.0 981,1 1827.2 1.09 2,.29 -.86 1912.50 7080.0 1024.9 1897.3.26 1.45 -.71 1913.00 7057.2 1048.3 1980,1 -.75.78 -o 28 1913.50 7043.2 1036.1 2016.7 -.46 -,40 -1,82 1914000 7037.6 994.1 2039.6 -.18 -1.40 -2,28 1914.50 7023.1 994,5 2107.9 -.48 -1.65 -077 1915.00 6992.2 904,3 2235.9 -1.02 -1.34 1,21

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0630.00.0 o0.0 0630o50 - 78.5 - 24.7 91.4 -2.61 -.82 2.74 0631,00 - 309.6 -60.1 182.8 -7.70 - 1.18 7.79 0631.50 - 511,8 - 115.3 274.3 -6.73 - 1.83 6.98 0632.00 - 647.6 -223,0 365,7 -4.52 - 3.58 5.77 0632.50 - 719.6 - 360.3 457.2 -2.39 - 4.57 5.16 0633.00 - 769.6 -484.6 548.6 -1.66 - 4,14 4.46 0633.50 - 822.3 - 610.7 640.0 -1.75 - 4.20 4.55 0634.00 - 853.0 -715.8 731.5 -1.02 - 3.50 3,64 0634.50 - 877.1 -815.0 822.9 -.80 - 3.30 3.40 0635.00 - 887.2 - 918.7 914.4 -.33 - 3.45 3,47 0635050 - 877.7 -1031.3 1005,8.31 - 3.75 3.76 0636.00 - 875,1 - 1157.1 1097,2.08 - 4.19 4o19 0636.50 - 890.2 -1295.3 1188.7 -.50 - 4.60 4o63 0637.00 - 918.5 - 1458.6 1280,1 -.94 - 5.44 5o52 0637,50 - 934.6 -1672.3 1371.6 -.53 - 7.12 7.14 0638.00 - 939.6 -1901.2 1463.0 -.16 - 7,62 7.63 0638.50 - 925.7 -2139.1 1554.4.46 - 7.92 7.94 0639.00 - 905.4 -2346.5 1645.9.67 - 6.91 6.94 0639.50 - 911.5 -2504.3 1737,3 -.20 - 5.25 5.26 0640.00 - 92-9 6 -2669.6 1828.8 -.60 - 5.50 5.54 0640.50 - 967.6 - 2842.3 1920.2 -1.26 - 5.75 5.89 0641,00 -1013.7 -2977.7 2011,6 -1o53 - 4.51 4.76 0641.50 -1001.4 -3119,1 2103.1.40 - 4.71 4.72 0642.00 - 980.4 - 3247.4 2194.5.69 - 4.27 4o33 0642.50 - 952.5 - 3388.7 2286.0.93 - 4.71 4.80 0643.00 - 926.3 - 3556.2 2377.4.87 - 5.58 5.65 0643.50 - 858.5 -3718.4 2468.8 2.26 - 5.40 5.86 0644.00 - 755.1 -3884.9 2560.3 3.44 - 5,54 6.53 0644.50 - 655.8 -4094.2 2651.7 3., 31 - 6.97 7.72 0645 o00 - 576.9 4267.1 2743.2 2,62 - 5.76 6.33 0645.50 - 464.5 -4494.9 2834,6 3.74 - 7.59 8.46 0646.00 - 340.0 -4744.0 2926.0 4.14 - 8,30 9.28 0646.50 - 139.1 -4980.5 3017.5 6.69 - 7.88 10.34 0647.00 90.9 - 5214.5 3108.9 7.67 - 7.79 10.93 0647.50 303.2 - 5424.7 3200,4 7.07 - 7.00 9.95 0648.00 481.1 - 5612.7 3291.8 5.92 - 6.26 8.62 0648.50 727.1 - 5838.5 3383.2 8.20 - 7.52 11.13 0649000 979.2 -6113.9 3474.7 8,40 - 9 17 12.44 0649050 120400 -6411.4 3566.1 7.49 - 9o91 12,43 0650000 1418.4 -6731,0 3657.6 7.14 -10.65 12,82

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0700000.0.0.0 0700.50 - 108.4 - 10.2 91.4 -3.61 -.34 3.63 0701.00 - 317.8 - 9.9 182.8 -6.97.00 6.97 0701.50 - 518.8 - 39.0 274.3 -6.69 -.96 6.76 0702.00 - 626.2 - 137.6 365.7 -3.58 - 3.28 4.86 0702.50 - 707.5 - 254.7 457.2 -2.70 - 3.90 4.74 0703o00 - 754.8 - 364.8 548.6 -1.57 - 3.67 3.99 0703.50 - 788.1 - 482.9 640.0 -1.11 - 3.93 4o09 0704.00 - 811.2 - 602.5 731.5 -.77 - 3.98 4.05 0704.50 - 837.0 - 719.9 822.9 -.85 - 3.91 4.00 0705.00 - 850,1 - 841,2 914.4 -.43 - 4.04 4.06 0705.50 - 861.4 - 956.7 1005.8 -.37 - 3.84 3.86 0706.00 - 870.4 -1102.1 1097.2 -.30 - 4.84 4.85 0706.50 - 889.7 -1261.3 1188.7 -.64 - 5.30 5.34 0707.00 - 914.6 -1498.4 1280,1 -.82 - 7.90 7094 0707.50 - 916.2 -1723.1 1371.6 -.05 - 7.49 7.49 0708.00 - 886.0 -1944.3 1463.0 1.00 - 7.37 7.44 0708050 - 868.8 -2172.3 1554.4.57 7. 60 7.62 0709.00 - 860.2 -2363o5 1645.9.28 - 6.37 6.37 0709.50 - 879,8 -2526.4 1737.3 -.65 - 5.43 5,47 0710.00 - 927.4 -2693,4 1828.8 -1.58 - 5.56 5.78 0710.50 - 987.4 -2835.5 1920.2 -2.00 - 4.73 5,14 0711o00 -1024.1 -2974,1 2011.6 -1.22 - 4.62 4.77 0711.50 -1017.7 -3113,8 2103.1.21 - 4.65 4.65 0712.00 - 997.5 -3283,3 2194.5.67 - 5.65 5.69 0712.50 - 995.1 -3447.5 2286,0.08 - 5.47 5,47 0713000 - 963.3 -3620.2 2377.3 1,06 - 5.75 5.85 0713050 - 905.0 -3799.0 2468.8 1.94 - 5.95 6.26 0714o00 - 810.6 -3984.0 2560,3 3.14 - 6.16 6.92 0714.50 - 732.4 -4196.7 2651.7 2.60 - 7.08 7.55 0715000 - 648.8 -4393.9 2743.2 2.78 - 6.57 7.13 0715050 - 552.0 -4629.3 2834.6 3.22 - 7.84 8.48 0716o00 - 436.3 -4889.0 2926,0 3.85 - 8.65 9.47 0716.50 - 256.1 -5158.5 3017.5 6.00 - 8.98 10.80 0717.00 - 75.8 -5428,0 3108.9 6.00 - 8.98 10.80 0717.50 108.0 -5678.7 3200.3 6.16 - 8.35 10.38 0718.00 277.4 -5883.4 3291.8 5.61 - 6.82 8.83 0718050 484.8 -6160.6 3383.2 6,91 - 9.23 11.53 0719000 691.4 -6470.7 3474.7 6.88 -10.33 12.42 0719050 901.5 -6816.7 3566.1 7.00 -11.53 13.49 0720.00 109501 -7157.4 3657.6 6.45 -11.35 13006

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0730.00.0.0 o0 0730,50 - 98,0 o 1 91,4 -3.26.00 3.26 0731.00 - 313.2 24,6 18208 -7.17.81 7.21 0731.50 - 551.0 41.4 274.3 -7.92.55 7.94 0732.00 - 733.5 3.8 365.7 -6.08 - 1.25 6.21 0732.50 - 839.9 - 97.1 457.2 -3.54 - 3.36 4.89 0733.00 - 881.2 - 209.9 548.6 -1.37 - 3.75 4.00 0733.50 - 921.8 - 315.6 640.0 -1.35 - 3.52 3.77 0734.00 - 965.1 - 429.6 731.6 -1.44 - 3.80 4.06 0734.50 - 984.1 - 552.2 82209 -.63 - 4.08 4.13 0735.00 - 987.7 - 651.2 914.4 -.11 - 3,29 3.30 0735,50 - 979.2 - 756.8 1005.8 -.28 - 3.52 3.53 0736.00 - 999.4 - 893.5 109702 -.67 - 4.55 4.60 0736.50 -1019.7 -1055.9 1188.7 -.67 - 5.41 5.45 0737.00 -1027.4 -1268.7 1280.1 -.25 - 7.09 7.09 0737.50 -1003.9 -1534,1 1371.6.78 - 8.84 8.88 0738.00 - 980.8 -1784.1 1463.0.76 - 8,33 8.36 0738.50 - 931.1 -2024.4 1554.4 1.65 - 8.00 8,17 0739.00 - 869,9 -2231.2 1645,9 2.04 - 6,89 7.18 0739.50 - 845.9 -2402,2 1737.3.79 - 5,70 5.75 0740.00 - 859.0 -2582.3 1828.8 -.43 - 6.00 6.02 0740.50 - 920.5 -2751.2 1920.2 -2,05 - 5.62 5.98 0741.00 - 970.3 -2916.9 2011.2 -1.66 - 5.52 5.76 0741050 -1006.9 -3117.3 2103.1 -1 21 - 6,67 6.78 0742.00 -1009.1 -3321.5 2194.5 -.07 - 6.80 6.80 0742.05 - 996.1 -3520.1 2286.0.43 - 6,62 6o.63 0743000 - 962.8 -3696.1 2377.4 1.11 - 5.86 5.97 0743.50 - 899.2 -3894.9 2468.8 2.11 - 6.62 6.95 0744.00 - 819.4 -4063.7 2560.3 2.66 - 5.62 6.22 0744.50 - 734.8 -4299.0 2651.7 2.81 - 7.84 8.33 0745.00 - 666.9 -4516.4 2743.2 2.26 - 7.24 7,59 0745.50 - 578.1 -4777.3 2834.6 2.96 - 8.69 9.18 0746.00 - 483.8 -5024.4 2926.0 3.14 - 8.23 8.81 0746.50 - 370.6 -5298.8 3017.6 3.77 - 9.14 9,89 0747.00 - 234.9 -5603.7 3108.9 4.52 -10.16 11.12 0747.50 - 51,6 -5918.7 3200.4 6.10 -10.50 12.14 0748.00 97.6 -6216.4 3291.8 4.97 - 9.92 11.09 0748.50 270.9 -6465.9 3383.2 5.77 - 8.31 10.12 0749.00 448.0 =6746.1 3474.7 5.90 - 9.34 11.05 0749050 614.4 -7090.2 3566.1 5054 -11.46 12.73 0750C00 79303 -7423.8 365706 5096 -11.11 12.61

Single Theodolite Data -8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0800.00.0 o 0 o0 0800.50 - 138.1 3.6 91.4 -4,60.12 4,60 0801.00 - 304.0 30.3 182.8 -5.53.89 5.60 0801.50 - 434.0 53.2 274.3 -4.33.76 4.39 0802.00 - 661.0 75.3 365.7 -7.56.73 7.60 0802.50 - 860.3 73.7 457.2 -6.64 -.05 6.64 0803000 - 977.6 - 3.4 548.6 -3.91 -2.57 4.68 0803.50 -1030.8 - 106.5 640.0 -1.77 -3.43 3.86 0804 00 -1068.6 - 207.7 731.5 -1.25 -3.37 3.59 0804.50 -1092.6 - 282.5 822.9 -.7.9 -2.49 2,62 0805.00 -1106,3 - 355o,2 914.4 -.45 -2.42 2.46 0805,50 -1124.8 - 449.9 1005.8 -.61 -3.15 3.21 0806000 -1145.4 - 6115 1097.2 -.68 -5,38 5.43 0806.50 -1148.7 - 837.6 1188.7 -.11 -7.53 7.53 0807.00 -1115.2 -1080 7 1280 o 1 1.11 -8.10 8.17 0807 50 -1073.5 -1325.7 1371.6 1.38 -8.16 8.28 0808.00 -1025.8 -1526.6 1463.0 1.59 -6.69 6.88 0808.50 - 999.0 -1695.9 1554.4.89 -5.64 5.71 0809000 -1030.4 -18;28.7 1645.9 -1.04 -4.42 4.55 0809.50 -1092.7 -1955.1 1737.3 -2.07 -4,21 4.69 0810,00 -1160.7 -2111.3 1828.8 -2.26 -5.20 5.67 0810 50 -1206.3 -2297.6 1920 2 -1.51 -6.21 6.39 0811o00 -1226.9 -2493,4 2011.6 -.68 -6.52 6.56 0811050 -1227.5 -2668.8 2103.1 -.01 -5.84 5.84 0812.00 -122005 -2861,5 2194.5.23 -6,42 6.42 0812,50 -1195.6 -3050.9 2286.0.82 -6.31 6.36 0813,00 -1174.8 -3281.1 2377.4.69 -7.67 7.70 0813 50 -1151.9 -3503.4 2468.8.76 -7 40 7.44 0814,00 -1100.6 -3739.1 2560.3 1.71 -7.85 8.04 0814, 50 -1042.2 -4029.8 2651.7 1.94 -9. 69 9.88 0815.00 - 953.9 -4302.6 2743.2 2.94 -9.09 9.55 0815,50 - 87204 -4617.3 2834.6 2.71 -10.48 10.o83 0816000 - 717.1 -4915.4 2926.0 5.17 -9.93 11020 0816,50 - 589.3 -5172.0 3017.5 4.26 -8.5 5 9.55 0817000 - 427.6 -5433.7 3108.9 5.38 -8.72 10.25 0817,50 - 298.6 -5695.2 3200.4 4.30 -8.71 9072 0818000 - 156.7 -5985.o 7 3291.8 4.72 -9.68 10.77 0818.50 - o0 -6257.2 3383.2 5.22 -9 04 10.44 0819.00 136 o8 -6533.5 3474,7 4. 56 -9,21 10.27 0819.50 258.9 -6832.7 3566.1 4.07 -9.97 10.77 0820.00 397,2 -710508 3657.6 4060 -9o10 10.20

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0830.00.0.0.0 0830.50 - 55.5 14.1 91,4 -1.85.47 1.91 0831.00 -126.9 6,2 182,8 -2.37 -.26 2.39 0831.50 -251.5 19.3 274.3 -4.15.43 4.17 0832.00 -407.3 15.6 365.7 -5.19 -.12 5.19 0832.50 -528.1 -39.7 457.2 -4.02. -1.84 4.43 0833.00 -599.4 - 120.8 548.6 -2.37 -2.70 3,59 0833.50 -654,1 - 199,9 640,0 -1.82 -2.63 3.20 0834.00 -704.6 - 263,4 731.5 -1.68 -2.11 2,70 0834.50 -734.5 - 331.6 822.9 -.99 -2.26 2.48 0835.00 -782.7 - 428.6 914o4 -1.60 -3.22 3.60 0835.50 -814.7 - 589.7 1005.8 -1.06 -5.37 5.48 0836.00 -830.1 - 793.2 1097.2 -.51 -6.78 6.80 0836.50 -819,2 -1011,6 1188,7.36 -7.28 7.27 0837.00 -790.8 -1217.7 1280.1.94 -6.86 6.93 0837.50 -7584 -1402 o 7 13716 1.07 -6.16 6.25 0838.00 -731.9 -1555.4 1463.0.88 -5.09 5.16 0838 o 50 -765.3 -1687.9 1554.4 -1.1 o1 -4 -38 4.52 0839.00 -825.2 -1802.5 1645.9 -1.99 -3.84 4.33 0839.50 -892.9 -195902 1737.3 -2.25 -5.22 5.68 0840.00 -948,9 -2121.4 1828,8 -1.86 -5.40 5.71 0840.50 -959.8 -2272,2 1920.2 - o36 — 5 02 5.04 0841.00 -978.4 -2483.8 2011.6 -.61 -7.05 7.07 0841.50 -966.3 -2683 9 2103.1.40 -6.67 6.68 0842 o 00 -950.4 -2890.5 2194.5.53 -6.88 6.90 0842.50 -961.8 =3107.1 2286.0 -.38 -7.21 7.22 0843.00 -944.1 -3314.4 2377.3 o 58 -6.90 6.93 0843.50 =917 o1 -3572.0 2468.8.89 -8,58 8,63 0844.00 -863,4 -3831.4 2560,3 1.79 -8.64 8.82 0844.50 -800. o4 -4117.5 o 2651.7 2.10 -9 53 9.76 0845.00 -687.1 -4388.1 2743.2 3.77 - 9 o 01 9 77 0845.50 -580.8 -4662.9 2834.6 3.54 -9.16 9.82 0846.00 -474.2 -4924.9 2926.9 3.55 -8.73 9,42 0846.50 -381,2 -5191.4 3017.5 3,09 -8.88 9.41 0847.00 -287.6 -5487.6 3108.9 3.12 -9.86 10.34 0847.50 -181,3 -5770.8 3200,4 3.54 -9.44 10.08 0848.00 -105.8 -6061.8 3291.8 2.51 -9.70 10.02 0848.50 - 22.3 -6389.8 3383.2 2.78 -10.93 11.28 0849.00 93.1 =6674.2 3474.7 3.84 -9,47 10.23 0849.50 193.7 -6968.1 3566,1 3.35 -9.79 10.35 0850o00 317ol -726503 3657.6 4.11 -9.90 10.72

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity _Time X Y Z U V VT 0900,00 0.0.0 0 0900,50 - 66.3 29 1 91.4 -2.21.97 2.41 0901.00 -121.0 30'.1 182.8 -1.82.03 1.82 0901.50 -208.6 33 0 274.3 -2.92.09 2.92 0902.00 -346,6 44.4 365.7 -4.60.37 4.61 0902.50 -496.8 171.3 457.2 -5.00 -.90 5.08 0903,00 -593.3 -38.3 548.6 -3.21 -1.85 3.71 0903.50 -659.6 - 102.1 640.9 -2.20 -2.12 3,06 0904.00 -711.8 - 168.2 731.5 -1.74 -2.20 2.81 0904.50 -741.7 - 216.8 822.9 -.99 -1.62 1.90 0905.00 -761.6 - 272.6 914.4 -.66 -1.86 1.97 0905.50 -791.1 - 372.2 1005,8 -.98 - 3.31 3.46 0906.00 -795.4 - 526.4 1097.2 -.14 -5.13 5.14 0906,50 -744.8 - 731.9 1188.7 1.68 -6.85 7.05 0907.00 -744,8 - 869.0 1280.1 -.00 -4.56 4.56 0907.50 -711.1 -1030.9 1371.6 1.12 -5.39 5.51 0908.00 -691.0 -1187.4 1463.0.66 -5.21 5.25 0908.50 -702.4 -1326.6 1554.4 -.37 -4.64 4.65 0909,00 -744.4 -1442.3 1645.9 -1,40 -3.85 4o10 0909.50 -809,9 -1523.3 1737.3 -2.18 -2.70 3.47 0910o00 -862.0 -1641,9 1828.8 -1,73 -3.95 4,31 0910,50 -899.7 -1804.5 1920.2 -1.25 -5.42 5.56 0911.00 -927.8 -1989,6 2011.6 -.93 -6.16 6,23 0911.50 -926.1 -2171,2 2103.1.05 -6.05 6.05 0912.00 -930.0 -2385.5 2194.5 -.13 -7.14 7.14 0912.50 -955,3 -2582.4 2286.0 -.84 -6.56 6.61 0913.00 -943.1 -2802.4 2377.4.40 -7.33 7.34 0913.50 -930.5 -3043.7 2468.8.41 -8.04 8.05 0914.00 -897.3 -3302.7 2560.3 1,10 -8.63 8 o 70 0914,50 -867.7 -3586.8 2651.7.98 -9.47 9.52 0915.00 -786.9 -3867.6 2743.2 2.69 -9.36 9 o 74 0915.50 -739.1 -4234.9 2834.6 1.59 -12,24 12.34 09160.00 -627.6 -4410.0 2926.0 3.71 -5.83 6.92 0916.50 -542.3 - 4687.0 3017.5 2.84 -9.23 9.66 0917.00 -450.9 -4954.8 3108.9 3.04 -8.92 9,43 0917.50 -384.9 -5228.9 3200.4 2.23 -9.13 9.40 0918.00 -346.7 -5511.1 3291.8 1.24 -9.40 9.48 0918050 -304.2 -5805.0 3383.2 1.41 -9.79 9.89 0919o00 -202.8 -6113.2 3474.7 3.38 -10.27 10.81 0919050 -109.5 -6415.4 3566.1 3.10 -10.07 10.54 0920000 - 11.8 -6736.4 3657.6 3.25 -10.69 11.18

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 0930.00.0.0.0 0930.50 - 124.2 20.1 91.4 -4.14.67 4.19 0931.00 - 249.7 9.1 182.8 -4.18 -.36 4.19 0931.50 - 388.4 - 18.9 274.3 -4.62 -.93 4.71 0932.00 - 551.1 - 40.4 365.7 -5.42 -.71 5.47 0932.50 - 667,5 - 59.5 457.2 -3.88 -.63 3,93 0933.00 - 764.3 - 85.7 548.6 -3.22 -.87 3.34 0933.50 - 853.4 - 119,9 640.9 -2.97 -1.14 3.18 0934.00 - 900,7 - 102,6 731.5 -1.57.- 57 1.67 0934.50 - 935.5 - 144.8 822.9 -1.16 -1.40 1.82 0935.00 - 990.2 - 208.6 914.4 -1.82 -2.12 2.80 0935.50 -1043.8 - 256.3 1005.8 -1.78 -1,59 2.39 0936.00 -1088.0 - 340.9 1097.2 -1.47 -2.81 3.18 0936.50 -1092.8 - 457.1 1188.7 -.15 -3.87 3.87 0937.00 -1116.9 539.9 1280.1 -.80 -2.75 2.87 0937.50 -1124.2 - 664.8 1371.6 -.24 -4.16 4o17 0938.00 - 1118.2 - 806.4 1463,0.20 -4.71 4.72 0938.50 -1105.5 - 961.0 1554.4.42 -5.15 5.16 0939.00 -1117.9 -1098.5 1645.9 -.41 -4.58 4.60 0939.50 -1151.0 -1204.4 1737.3 -1.10 -3.53 3.69 0940.00 -1207.5 -1254.8 1828.8 -1.88 -1.67 2.52 0940.50 -1273.8 -1356.4 1920.2 -2.20 -3.38 4.04 0941.00 -1336.7 - 1484.5 2011.6 -2.09 -4.26 4.75 0941.50 -1394.7 -1633.0 2103,1 -1.93 -4.95 5.31 0942.00 -1445.2 -1784.6 2194,5 -1.68 -5.05 5.32 0942.50 -1470.1 -1950.9 2286.0 -.83 -5.54 5,60 0943.00 -1497.1 -2130.1 2377.3 -.89 -5,97 6.04 0943 o 50 -1536.1 -2294.5 2468.8 -1.29 -5.48 5.63 0944.00 -1538.9 -2462.8 2560.3 -.09 -5.60 5.60 0944.50 -1567.3 -2692.8 2651.7 -.94 -7.66 7.72 0945.00 -1573.0 -2945,9 2743.2 -.18 -8.43 8 43 0945.50 -1567.8 -3228.7 2834.2.17 -9.42 9.42 0946.00 -1537 7 -3519.7 2926.0 1.00 -9.70 9.75 0946.50 -1500.0 -3808,0 3017.5 1.25 -9.60 9,.69 0947.00 -1442.4 -4095.9 3108.9 1.92 -9.59 9 78 0947.50 -1478.4 -4342.8 3200.4 -1.20 -8.23 8.31 0948.00 -1383.8 -4641.8 3291.8 3.15 -9.96 10'.45 0948.50 -1402.4 -4955.9 3383.2 -.61 -10.46 10.48 0949.0 o 0 -1387 9 -5252.9 3474.7.48 -9.90 9.91 0949.50 -1301.2 -5541.2 3566.1 2.89 -9.60 10 03 0950 o00 -1220 o 6 -5842, 4 3657 o 6 2 o 68 -10.04 10 o 39

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1000.00.0.0.0 1000.50 - 113.3 - 29.3 91.4 -3.77 -.97 3.90 1001.00 - 218.8 - 61.9 182.8 -3.51 -1.08 3,68 1001,50 - 268.7 6709 274.3 -1.66 -.20 1,67 1002.00 -318.9 - 60.8 365.7 -1.67.23 1.69 1002.50 - 357.4 - 91,1 457.2 -1.28 -1.00 1.63 1003,00 - 368.3 -123.2 548.6 -.36 -1.07 1.13 1003.50 - 409.4 -156.3 640.0 -1.36 -1.10 1.75 1004.00 - 446.0 -188.4 731.5 -1.21 -1.06 1.62 1004.50 - 480.9 -237.6 822.9 -1.16 -1.64 2.01 1005.00 - 496.3 -300,6 914.4 -.51 -2.09 2.15 1005. 50 - 519,8 - 353.2 1005.8 -.78 -1.75 1.92 1006.00 - 551.6 -429.4 1097.2 -1.05 -2.53 2.74 1006.50 - 576.3 -513.5 1188.7 -.82 -2.80 2.92 1007.00 - 603,0 -617.9 1280.1 -.88 -3.48 3.59 1007.50 - 642.8 -684.6 1371.6 -1.32 -2.22 2.58 1008.00 - 687.0 -744.5 1463.9 -1.47 -1.99 2.47 1008.50 - 767.4 -822.9 1554,4 -2.68 -2.61 3,74 1009.00 - 857.9 -933.0 1645.9 -3.01 -3,66 4.75 1009.50 - 946.8 -1040.6 1737.3 -2.96 -3.58 4.65 1010.00 -1022,0 -1159.2 1828.8 -2.50 -3.95 4.68 1010.50 -1079.8 -1296.0 1920.2 -1.92 -4.56 4,95 1011.00 -1127.2 -1458.4 2011.6 -1 58 -5.41 5,64 1011.50 -1174.6 -1604.8 2103.1 -1.57 -4.87 5.12 1012.00 -1204.8 -1779.5 2194.5 -1.00 -5.82 5.90 1012.50 -1246,4 -1964.1 2286.0 -1.38 -6.15 6,30 1013,00 -1265.2 -2182.6 2377,4 -.62 -7.28 7.31 1013.50 -1282.7 -2412.5 2468.8 -.58 -7.66 7.68 1014,00 -1272.6 -2656.1 2560.3.33 -8.12 8.12 1014.50 -1260.1 -2898.1 2651.7.41 -8.06 8.07 1015.00 -1238,2 -3127.2 2743.2.73 -7,63 7.67 1015.50 -1236.3 -3342.2 2834.6.06 -7.16 7.16 1016000 -1243.3 -3590.3 2926.0' -.23 -8.27 8.27 1016.50 -1215.2 -3830.8 3017.5.93 -8.01 8.06 1017000 -1170.8 -4083.2 3108.9 1.47 -8.41 8.54 1017.50 -1135.2 -4357 o 9 3200,4 1.18 -9.15 9.23 1018.00 -1065.4 -4614.9 3291.8 2.32 -8.56 8.87 1018,50 - 963.3 -4865.2 3383.2 3.40 -8.34 9.01 1019o00 - 835.6 -5102.9 3474.7 4.25 -7.92 8,99 1019.50 - 685.2 -5380,4 3566.1 5.01 -9.25 10.52 1020.00 - 520.2 -5608o1 3657,6 5.49 -7.58 9.36

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1030.00.0.0.0 1030.50 - 12.0 -10o4 91.4 -.40 - o34.53 1031.00 - 45,9 11.4 182.8 -1.12.73 1.34 1031.50 - 79.7 33.3 274,3 -1.12.73 1.34 1032,00 -127.0 16,4 365,7 -1.57 - o56 1.67 1032.50 -166,1 8.4 457,2 -1o30 -.26 1.33 1033.00 -209.2 10.6 548,6 -1.43.07 1.43 1033o50 -224.9 28.0 640.0 -.52.58.78 1034.00 -247.5 -2.5 731.6 -.75 -1,02 1.25 1034.50 -290,4 -49,6 822.9 -1.42 -1.56 2.12 1035.00 -335.7 -108.4 914.4 _1.51 -1.95 2.47 1035.50 -384,3 -160.7 1005,8 -1.62 -1.74 2,38 1036,00 -432.9 -183.7 1097.2 -1.61 -.76 1,79 1036,50 -505,6 -201'.2 1188.7 -2.42 -.58 2.49 1037.00 -577.6 -236 9 1280,1 -2.40 -1.18 2.67 1037.50 -660.9 -308. 2 1371.6 -2.77 -23 o 3.65 1038.00 -743.6 -378.8 1463.9 -2.75 -2.35 3.62 1038.50 -836,3 -455.9 1554.4 -3.09 -2.57 4.02 1039.00 -918,1 -547.2 1645,9 -2.72 -3.04 4.08 1039o50 -1006.9 -666.4 1737.3 -2.95 -3.97 4.95 1040.00 -1101.5 -794.4 1828 8 -3.15 -4.26 5.30 1040.50 -1182 o 2 -923 6 1920.2 -2.68 -4.30 5.07 1041.00 -1248.3 -1073.6 2011.6 -2.20 -5.00 5.46 1041.50 -1346,1 -1246.5 2103,1 -3.26 -5.76 6.62 1042.00 -1436.8 -1216,9 2194,5 -3,02 -5.67 6.43 1042 50 -1500.6 -1598.9 2286.0 -2.12 -6 03 6,40 1043.00 -1532o3 -1806,8 2377.4 -1.05 -6,96 7,04 1043.50 -1540,1 -2007.1 2468,8 -.25 -6.67 6 68 1044,00 -1542.1 -2202.3 2560,3 -.06 -6,50 6.50 1044. 50 -1537 4 -2404. 9 2651.7 o 15 -6 o 72 6.o 72 1045,00 -1543.6 -2589.5 2743.2 -.20 -6.18 6,18 104550 - 1553.3 -2802.2 2834,6 -.32 -7.09 7 09 1046 00 -1533,7 -3023.0 2926,0.65 -7.36 7.39 1046.50 -1525 7 -3242.3 3017.5.26 -7.30 7.31 1047 00 -1509o2 -3470,9 3108.9.55 -7 62 7.64 1047.50 -1457.6 -3719.3 3200,4 1.72 -8.27 8.45 1048.00 -1399.5 -3974.1 3291.8 1.93 -8.49 8.71 1048.50 -1303o8 -4211.9 3383.2 3.18 -7,92 8.54 1049.00 -1193.4 -4453,9 3474.7 3.67 -8.06 8.86 1049.50 -1054,8 -4720,7 3566,1 4,62 -8,89 10,02 1050o00 -915o5 -4988.0 3657o6 4 o 64 -8,90 10 04

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1230.00.0.0.0 1230.50 - 70.1 28.3 91.4 -2.33.94 2.52 1231.00 - 117.7 3009 182.8 -1.58.08 1.58 1231.50 - 165.3 33.6 274.3 -1.58.08 1.58 1232.00 - 230.6 33.2 365.7 -2.17 -.01 2.17 1232.50 - 314.9 31.9 457.2 -2.81 -.04 2.81 1233.00 - 384.2 32.2 548.6 - 2.30.00 2.30 1233.50 - 451,4 - 6.2 640.0 -2,24 -1o28 2.58 1234.00 - 553.8 - 38.7 731.6 -3.41 -1o08 3.58 1234.50 - 655.1 - 108.4 822.9 -3.37 -2.32 4.09 1235.00 - 759.8 - 106.7 914.4 -3.48.05 3.48 1235.50 - 848.2 - 54.8 1005.8 -2.94 1.73 3.41 1236.00 894.6 - 24.9 1097.2 -1.54.99 1.83 1236.50 - 936.0 - 72.0 1188.7 -1.38 -1.56 2.08 1237.00 - 987.0 - 69.0 1280.1 -1.69.10 1.70 1237.50 -1067,2 - 33.5 1371.6 -2.67 1.18 2.92 1238.00 -1159.6 - 6.0 1463,0 -3.07.91 3,21 1238.50 -1263o2 6.6 1554,4 -3.45 - 42 3.48 1239,00 -1376.1.0 1645.9 -3.76 - 22 3,77 1239. 50 -1499.4 - 20.9 1737.3 -4.10 -.69 4.16 1240.00 -1605,3 - 64.4 1828.8 -3.52 -1.45 3,81 1240.50 -1718.3 - 126.1 1920.2 -3.76 -2.05 4.29 1241,00 -1820.6 - 111.3 2011.6 -3.41.49 3,44 1241.50 -1917,9 - 188.0 2103.1 -3.24 -2.55 4.12 1242.00 -1996,3 - 294.7 2194.5 -2,61 -3.55 4.41 1242,50 -2041,8 - 396.8 2286.0 -1,51 -3,40 3.72 1243.00 -2051.6 - 496.3 2377.4 -.32 -3.31 3.33 1243.50 -2081,7 - 581.2 2468.8 -1.00 -2.82 3.00 1244.00 -2101.8 - 731,9 2560.3 -.67 -5,02 5.06 1244050 -2139.4 - 882,8 2651.7 -1.25 -5.02 5.18 1245.00 -2177.0 -1033.6 2743.2 -1.25 -5.02 5.18 1245.50 -2220.9 -1220.9 2834.6 -1.46 -6.24 6.41 1246.00 -2218,6 -1386.3 2926.0.07 -5.51 5.51 1246.50 -2196,9 -1549.7 3017.5.72 -5.44 5.49 1247.00 -2149.6 -1716.0 3108.9 1,57 -5.54 5.76 1247.50 -2090.9 -1909.2 3200.4 1.95 -6.44 6.73 1248.00 -2041.9 -2106.1 3291.8 1.66 -6.56 6.77 1248.50 -1967,4 -2311.7 3383.2 2.45 -6.85 7.27 1249.00 -1902.6 -2497.4 2474 7 2.16 -6.19 6.55 1249050 -1809,6 -2680.3 3566,1 3,09 -6.09 6.83 1250.00 -1710.1 -2868.7 3657.6 3.31 -6,28 7o10

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1300.00 0.0.0.0 1300.50 - 78.9 - 89.8 91.4 -2,63 -2.99 3.98 1301.00 -141.0 - 115.4 182,8 -2.06 -.85 2.23 1301.50 -205,5 - 108.8 274.3 -2.15.21 2.16 1302,00 - 268.6 - 84.6 365.7 -2,10.80 2,25 1302.50 -323.3 - 86,0 457.2 -1,82 -.04 1.82 1303,00 -390,5 - 99.6 548.6 -2,23 -.45 2.28 1303 50 -459.2 - 108.5 640.9 -2.29 -.30 2.31 1304.00 -553.4 - 104.5 731.5 -3.14.13 3.14 1304. 50 -647.2 - 80.6 822.9 -3.12.79 3.22 1305.00 - 753 9 - 61.9 914.4 -3.55.62 3.60 1305.50 -794.1 - 19,3 1005.8 -1.34 1.41 1.95 1306.00 -847.8 20.7 1097.2 -1,78 1.33 2.23 1306.50 - 908 1 34.8 1188.7 -2.01.47 2.06 1307.00 -966,6 54.0 1280,1 -1.94.63 2.05 1307.50 -1029.9 86.4 1371.6 -2,10 1.08 2.37 1308.00 -1120,0 121.6 1463.0 -3,00 1.17 3.22 1308.50 -1223.8 141.6 1554.4 -3.45.66 3.52 1309.00 -1340.9 138.4 1645.9 -3.87 -.10 3.87 1309.50 - 1456.4 137.6 1737.3 -3,88 -.02 3.88 1310,00 -1574.1 118.3 1828.8 -3,92 -.64 3.97 1310.50 -1665,3 113.5 1920,2 -3.04 -.16 3.04 1311.00 -1764.5 98.6 2011.6 -3.30 -.49 3,34 1311.50 -1847o4 29.0 2103.1 -2.76 -2.32 3.60 1312,00 -1920.4 - 53.6 2194.5 -2.43 -2.75 3.67 1312.50 - 1941,9 - 132.3 2286.0 -.68 -2.62 2.71 1313.00 -1942.5 - 200.7 2377.4 -.04 -2,28 2,28 1313.50 -1949.2 - 291.2 2468.8 -.22 -3.01 3.02 1314.00 -1947.3 - 424.5 2560.3.06 -4.44 4.44 1314.50 -1962.0 - 566.2 2651.7 -.48 -4.72 4.74 1315.00 -1991.0 - 728.6 2743.2 -.96 -5,41 5.49 1315.50 -2028.9 - 907.5 2834.6 -1.26 -5.96 6.09 1316.00 -2023. 9 -1080.6 2926.0.16 -5.76 5.77 1316.50 -1989.-2 -1233.3 3017.5 1.16 -5.09 5,22 1317o 00 -1948. 6 -1420.8 3108 9 1,35 -6.24 6.39 1317.50 -1902.9 -1608.0 3200.4 1.51 -6.24 6.42 1318.00 -1843..8 -1792.9 3291.8 1.97 -6.16 6.47 1318,50 -1768. 2 -19775 3383.2 2.51 -6,15 6,64 1319.00 -1677.3 -2146 9 3474.7 3,02 -5.64 6.40 1319.50 -1581.1 -2327.4 3566.1 3.20 -6.01 6.81 1320,00 -1481.0 -2504.2 3657.6 3.33 -5.89 6.77

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1600,00.0.0.0 1600,50 171.8 - 90.6 91.4 5.72 -3.02 6.47 1601.00 292.9 -160.4 182.8 4.03 -2.32 4.65 1601.50 355.0 -191.9 274.3 2.06 -1.05 2.32 1602o00 356.2 -234.9 365 o 7.03 -1.43 1.43 1602o50 325,9 -279.3 457.2 -1.00 -1.48 1.79 1603000 323,2 -325.6 548.6 -.09 -1.53 1.53 1603.50 344.3 -382,4 640.9.70 -1.89 2.02 1604.00 369.7 -373.6 731.5.84.29.89 1604.50 346.5 -366.4 822.9 -.77.24.81 1605.00 340.9 -358.0 914.4 -.18.27.33 1605.50 282.9 -300,2 1005.8 -1.93 1.92 2.73 1606o00 146,8 -259,4 1097,2 -4.53 1.35 4.73 1606.50 - 7.7 -261,2 1188.7 -5.15 -.05 5.15 1607 00 -149.2 -252.3 1280.1 -4.71.29 4,72 1607.50 -294,6 -252.5 1371.6 -4.84 -,00 4.84 1608.00 -402 o9 -208.4 1463.0 -3.57 1.47 3,87 1608.50 -469.4 -105.7 1554.4 -2,24 3.42 4.09 1609,00 -484.2 11.8 1645.9 -.49 3.92 3.95 1609.50 -507,2 119.9 1737.3 -.76 3.60 3.68 1610o00 -561.2 234.7 1828.8 -1.79 3.82 4.23 1610.50 -623.6 340.0 1920.2 -2.08 3.50 4.07 1611,00 -663.6 447.6 2011.6 -1.33 3.58 3.82 1611 50 -713.5 543.6 2103.1 -1.66 3.19 3.60 1612 00 -755.0 620,1 2194.5 -1.38 2.55 2.90 1612o50 -788.7 643.2 2286.0 -1.12.76 1,36 1613o00 -851.9 628.1 2377.4 -2.10 -.50 2,16 1613o50 -861.1 570.0 2468.8 -.30 -1.93 1.96 1614,00 -842.2 486.2 2560.3.63 -2.79 2,86 1614o50 -853.2 363,2 2651.7 -.36 -4,10 4.11 1615,00 -878.3 227.1 2743,2 -.83 -4.53 4,61

Single Theodolite Data - 8 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 2000.00.0.0.0 2000.50 2.2 - 71.9 91.4.07 -2.37 2.39 2001.00 - 66.5 -137.6 182.8 -2.29 -3.19 3.17 2001.50 - 171.0 -174.6 274.3 -3.48 -1.23 3.69 2002.00 - 284.1 -205.6 365.7 -3.77 -1.03 3.91 2002.50 - 407.7 -230.7 457.2 -4.12 -.83 4.20 2003.00 - 551.2 -244.2 548.'6 -4.78 -.45 4.80 2003,50 - 673.1 -271.9 640.0 -4.06 -.92 4.16 2004,00 - 804.6 -284.8 731.5 -4.37 -.43 4.39 2004.50 - 923.4 -298.2 822.9 -3.96 -.44 3.98 2005.00 -1047.3 -286.5 914.4 -4.13.39 4.15 2005.50 -1179.0 -259.2 1005.8 -4.38.90 4.48 2006.00 -1326.9 -222.0 1097.2 -4.92 1.23 5.08 2006.50 -1493.6 -186.0 1188.7 -5.55 1.20 5.68 2007.00 -1666.9 -157.6 1280.1 -5.77.94 5.85 2007.50 -1835.8 -125.1 1371.6 -5.63 1.08 5.73 2008.00 -1967.9 - 89.3 1463.0 -4.40 1.19 4.56 2008.50 -2018.3 - 28.1 1554.4 -1.67 2.03 2.64 2009.00 -1996.2 41.8 1645.9.73 2.33 2.44 2009.50 -1937.9 142.3 1737.3 1.94 3.34 3.87 2010.00 -1853.9 224.3 1828.8 2.79 2.73 3.91 2010.50 -1776.8 342.1 1920.2 2.56 3,92 4.69 2011,00 -1739.5 404.8 2011.6 1.24 2.08 2.43 2011,50 -1714.4 491.6 2103.1.83 2.89 3.01 2012.00 -1705.3 564,0 2194.5.30 2.41 2.43 2012.50 -1740.9 589.3 2286.0 -1.18.84 1.45 2013 00 -1820 2 605,5 2377.4 -2.64.54 2.69 2013.50 -1902,4 614.5 2468.8 -2.74.29 2.75 2014.00 -1952.6 578.4 2560.3 -1.67 -1o 2 2.06 2014.50 -1970,8 523.4 2651.7 -.60 -1.83 1.92 2015.00 -1980.1 479.0 2743.2 -.30 -1.48 1.51

Single Theodolite Data - 16 KM, Station Balloon Position Wind Velocity Time X Y Z U V VT 1700.00.0.0.0 1700.50 - 66.1 -29.5 91.4 -2.20 -.98 2.41 1701.00 - 134.6 -59.1 182.8 -2.28 -.98 2.48 1701o50 - 214.4 -90.1 274.3 -2.66 -1.03 2.85 1702.00 - 282.3 -72.8 365.6 -2.26.57 2.33 1702.50 - 350.2 -55.4 457.2 -2.26.57 2.33 1793.00 - 421.1 -49.4 548o6 -2.36.20 2.37 1703.50 - 514.8 -59.5 640,0 -3.12 -.33 3.14 1704000 - 613.9 -72.1 731.5 -3.30 -.41 3.32 1704.50 - 714.2 -72.5 822.9 -3.34 -.01 3.34 1705.00 - 802.0 -81o4 914.4 -2.92 -.29 2.94 1705.50 - 877,5 -72.1 1005.8 -2.51.31 2.53 1706,00 - 942.9 -39.5 1097.2 -2.17 1.08 2.43 1706,50 -1021.8 -35.6 1188.7 -2.62.12 2.63 1707.00 -1112.2 -36.8 1280.1 -3.01 -.04 3.01 1707.50 -1204.9 - 2.0 1371.6 -3.09 1.15 3.30 1708.00 -1279.9 46.9 1463.0 -2.49 1.63 2.98 1708.50 -1383.4 65.2 1554.4 -3.45.61 3.50 1709.00 -1462.5 107.4 1645.9 -2.63 1.40 2.98 1709.50 -1549.7 168.3 1737.3 -2.90 2.03 3.54 1710,00 -1632.0 293.6 1828.8 -2.74 4.17 4.99 1710.50 -1690.1 418.2 1920,2 -1.93 4.15 4.58 1711,00 -1666.4 509.4 2011.6.79 3.04 3.14 1711.50 -1643,4 607.9 2103.1.76 3.28 3.36 1712o00 -1645.0 705.1 2194.5 -.05 3.23 3.23 1712,50 -1698.9 735.2 2286.0 -1.79 1.00 2.05 1713.00 -1758.2 696.1 2377.4 -1.97 -1,30 2.36 1713.50 -1817.1 647.0 2468.8 -1.96 -1.63 2.55 1714o00 -1785.1 569.7 2560.3 1,06 -2.57 2 o 78 1714.50 -1792.1 485.6 2651.7 -.23 -2.80 2.81 1715.00 -1799.6 398.9 2743.2 -.25 -2.88 2.89

Single Theodolite Data - 16 KM Station Balloon Position Wind Veloc Time X Y Z U V VT 1730.00 - o0.0.0 1730o50 - 94,5 - 20.2 91.4 -3.15 -.67 3.22 1731,00 - 123.0 - 40.4 182.8 -.94 -.67 1.16 1731.50 - 180.5 - 51.7 274.3 -1.91 -.37 1.95 1732.00 - 257.8 - 75.4 365.7 -2.57 -.78 2.69 1732.50 - 355,1 -141.3 457.2 -3.24 -2.19 3.91 1733.00 - 477.8 -177.7 548.6 -4.08 -1.21 4.26 1733.50 - 613.4 -182.8 640.0 -4.51 -.17 4.52 1734.00 - 670.9 -168.5 731.5 -1.91.47 1.97 1734,50 - 719.4 -154.2 822.9 -1.61.47 1.68 1735.00 - 790,6 -125.2 914.4 -2.37.96 2.56 1735.50 - 874,4 - 71.8 1005.8 -2.79 1.77 3.31 1736.00 - 960.1 - 30.1 1097.2 -2.85 1.39 3.17 1736.50 -1036.8 16.2 1188.7 -2.55 1.54 2.99 1737.00 -1111.2 58.2 1280.1 -2.48 1.39 2.84 1737.50 -1238.5 112.7 1371.6 -4.24 1.81 4.61 1738.00 -1383.5 162.5 1463.0 -4.83 1.66 5.11 1738.50 -1506.6 217.1 1554,4 -4.09 1.81 4.48 1739.00 -1631.2 293.5 1645.9 -4.15 2.54 4.87 1739.50 -1752.9 375.8 1737.3 -4.05 2.74 4.89 1740.00 -1846.3 450,1 1828,8 -3.11 2.47 3.97 1740.50 -1953.0 501.4 1920.2 -3.55 1.71 3.94 1741.00 -2059.2 590.4 2011,6 -3.53 2.96 4.61 1741.50 -2147.3 689.4 2103.1 -2.93 3.29 4.41 1742.00 -2139.2 812.6 2194.5.26 4.10 4.11 1742.50 -2110.3 939.6 2286.0.96 4.23 4.34 1743.00 -2077.9 1067.9 2377.4 1.08 4.27 4.41 1743.50 -2084.3 1174.5 2468.8 -.21 3.55 3.55 1744.00 -2106.7 1260.8 2560.3 -.74 2.87 2.97 1744.50 -2133.7 1278.2 2651.7 -.89.57 1.06 1745o00 -2163.6 1279.5 2743.2 -.99.04.99

Single Theodolite Data - 16 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1800.00.0.0.0 1800.50 14.2 - 2.6 91.4.47 -.08.48 1801o00 4.7 -.6 182o8 -.31.06.32 1801.50 - 21.2 - 2.5 274.3 -.86 -.06.86 1802.00 - 47.3 - 4,4 365.7 -.86 -.06.86 1802.50 - 73.3 - 6.2 457.2 -.86 -.06.86 1803.00 - 99.3 - 8.1 548.6 - Z86 - o06.86 1803.50 -176.1 7.0 640.0 -2.55 o50 2.60 1804.00 -261.5 14.6 731.5 -2.84.25 2.85 1804.50 -342.8 31.2 822.9 -2.71.55 2.76 1805.00 -426.4 57.6 914. 4 -2.78.88 2.92 1805.50 -502,2 90.3 1005.8 -2.52 1.09 2.75 1806.00 -598.6 107.7 1097.2 -3.21.57 3.26 1806.50 -715.4 117.7 1188.7 -3.89.33 3.90 1807.00 -831.0 128.6 1280.1 -3.85.36 3.86 1830.00.0.0.0 1830.50 78,0 -42.5 91.4 2.60 1.41 2.96 1831.00 116.3 -69e0 182.8 1.27.88 1.55 1831. 50 106.2 -62.5 274.3 -.33.21.40 1832.00 53.7 -44.8 365.7 -1.75.59 1.84 1832o50 1.1 -27.1 457.2 -1.75.59 1.84 1833.00 - 84.1 -16.9 548.6 -2.84.34 2.86 1833.50 -169.4 - 6.6 640.0 -2.84.34 2.86 1834.00 -254.7 3.5 731,5 -2.84.34 2.86 1834.50 -372.4 43.7 822,9 -3.92 1.34 4.14 1835.00 -490.8 74.2 914.4 -3.94 1.01 4.07 1835o50 -608,2 113.8 1005.8 -3.91 1.31 4.12 1836.o 00 -716.3 149.6 1097 o 2 -3.60 1.1 o 9 3.79 1836.50 -817.7 170.8 1188.7 -3.38 ~ 70 3.45 1837.00 -941.1 194.9 1280.1 -4.11.80 44.19 1837 50 -1053.1 218.1 1371.6 -3.73 o 77 3.81 1838.00 -1148.3 248.3 1463.0 - 317 1.00 3,33 1838.50 -1229.9 288.4 1554.4 - 2.71 1.33 3.03

Single Theodolite Data - 16 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1900.00.0.0.0 1900.50 97.5 - 10.2 91.4 3.25 -.34 3.26 1901.00 131,1 - 38.9 182.8 1.12 -.95 1.47 1901.50 164.8 - 67.5 274.3 1.12 -.95 1.47 1902.00 109.2 - 78.5 365.7 -1.85 -.36 1.88 1902.50 49.4 - 107.4 457.2 -1.99 -.96 2.21 1903.00 - 31.8 - 114.2 548.6 -2.71 -.22 2.71 1903.50 - 92.4 - 118.3 640.0 -2.01 -.13 2.02 1904.00 - 181.8 - 112.7 731.5 -2.97.18 2.98 1904.50 - 280.3 - 73.5 822.9 -3.28 1.30 3.53 1905.00 - 394o7 - 26.9 914.4 -3.81 1.55 4.11 1905.50 - 521.2 10.9 1005.8 -4.21 1.26 4.40 1906.00 - 647.8 37,3 1097.2 -4.21.88 4.31 1906.50 - 784.3 61.7 1188.7 -4.55.81 4.62 1907.00 - 921.2 100,0 1280,1 -4.56 1.27 4.73 1907.50 -1054.5 140.7 1371.6 -4.44 1.35 4.64 1908.00 -1179.4 180.5 1463,0 -4.16 1.32 4.37 1908.50 -1310.5 212.2 1554.4 -4.36 1.05 4.49 1909.00 -1456.1 246,2 1645.9 -4.85 1.13 4.98 1909.50 -1520.0 345.3 1737.3 -2.13 3.30 3.93 1910.00 -1457.1 406.8 1828.8 2.09 2.04 2.93 1910.50 -1391.4 484.5 1920.2 2.18 2.59 3.39 1911.00 -1383.2 578.9 2011.6.27 3.13 3.14 1911.50 -1359.5 634.0 2103.1.79 1.84 2.00 1912.00 -1363.0 658.9 2194.5 -.11.83.83 1912.50 -1399.2 661.4 2286.0 -1.20.08 1.21 1913.00 -1453.3 677.7 2377.4 -1.80.54 1.88 1913.50 -1488.3 659.5 2468,8 -1.16 -.60 1.31 1914.00 -1487.9 583.6 2560,3.01 -2.52 2.52 1914.50 -1491,9 522.4 2651.7 -.13 -2.03 2.04

Single Theodolite Data - 16 KM Station Balloon Position Wind Velocity Time X Y Z U V VT 1930.00.0.0.0 1903.. 50 24.9 - 44.8 91.4.83 -1.49 1.71 1931.00 - 2.6 -101.3 182.8 -.92 -1.88 2.09 1931.50 - 61.6 -124.7 274.3 -1.96 -.78 2.11 1932.00 - 121.5 -143.3 365.7 -1.99 -.61 2.09 1932.50 - 187.6 -141.4 457.2 -2.20.06 2.20 1933.00 - 270.8 -126.8 548.6 -2.77.48 2.81 1933.50 - 355.5 -100.6 640.0 -2.82.87 2.95 1934.00 - 444.9 - 78.4 731.5 -2.97.73 3.06 1934.50 - 557.7 - 41.9 822.9 -3.75 1.21 3.95 1935.00 - 666.7 3.4 914.4 -3.63 1.51 3.93 1935.50 - 789.7 52.4 1005.8 -4.09 1.63 4.41 1936.00 - 921.4 103.3 1097.2 -4.39 1.69 4.70 1936.50 -1060.1 147.1 1188.7 -4.62 1.45 4.84 1937.00 -1185.6 170.8 1280.1 -4.18.79 4.25 1937.50 -1343.7 191.2 1371.6 -5.26.67 5.31 1938100 -1505.1 214.2 1463.0 -5.37.76 5.43 1938o50 -1673.1 241.1 1554.4 -5.60.89 5.67 1939.00 -1753.5 290.3 1645.9 -2.67 1.63 3.14 1939.50 -1826.9 365.0 1737.3 -2.44 2.49 3.49 1940.00 -1847.1 446.8 1828,8 -.67 2.72 2.80 1940.50 -1784.2 504.9 1920.2 2.09 1.93 2.85 1941.00 -1731.8 572.7 2011.6 1.74 2.26 2.85 1941.50 -1693.8 670.6 2103.1 1.26 3.26 3.50 1942.00 -1635.0 728.0 2194.5 1.95 1.91 2.73 1942.50 -1623.6 774,4 2286.0 o38 1.54 1.59 1943,00 -1639.6 799,7 2377.4 -.53.84.99 1943.50 -1644.7 795,1 2468.8 -.17 -.15.22 1944.00 -1688.4 812.6 2560.3 -1.45 o58 1.57 1944.50 -1736,7 803.2 2651.7 -1.60 -.31 1.63 1945.00 -1772.0 759.5 2743.2 -1.17 -1.45 1.87