Work Description

Title: A Statistical Analysis of High-frequency Transient-Large-Amplitude Geomagnetic Disturbances: Data Open Access Deposited

h
Attribute Value
Methodology
  • The data in this repository are transient-large-amplitude dB/dt intervals with second-timescale and amplitude > 6 nT/s. These dB/dt intervals are identified by the automated geomagnetic disturbance classifier described in detail in McCuen et al. (2023). This automated technique is run on yearly data files from individual magnetometer stations and saves the data product files that are in the filepath: 'prod_init/Products/"year"/' and have the filename structure: '"station code"/"year"/_algfinal_2-60s_6-1000nT_6-100nTs_xyz_filterf_svmvote_chk.csv'. The data within these files is structured with the columns: ['start time', 'end time', 'start B value', 'end B value', 'dB (change in magnetic field strength)', 'dt (change in seconds)', 'dbdt (change in B divided by change in seconds)', 'component', 'station code']. These data product files are created for a set of stations from five magnetometer arrays, the details of which are described in the instruments section below. All available data from these stations from the years of 2009 to 2019 were used and the data products saved in the yearly folders located at the filepath mentioned above.
Description
  • We present a comprehensive statistical analysis of high-frequency transient-large-amplitude (TLA) magnetic perturbation events that occurred at 12 high-latitude ground magnetometer stations throughout solar cycle 24 from 2009 to 2019. TLA signatures are defined as one or more second-timescale dB/dt interval with magnitude ≥ 6 nT/s within an hour event window. This study characterizes high-frequency TLA events based on their spatial and temporal behavior as well as relation to auroral substorms, geomagnetic storm phases and nighttime geomagnetic disturbance events events (GMD). We show that TLA events occur primarily at nighttime and solely in the high-latitude region above 60 degrees geomagnetic latitude. The largest TLA events occurred more often in the declining phase of the solar cycle when solar wind velocity was higher and ring current activity was lower, suggesting association to high-speed flows caused by coronal holes and subsequent corotating interaction regions reaching Earth. TLA perturbations often occurred preceding or within the most extreme nighttime geomagnetic disturbance (GMD) events with 5-10 minute timescales, but the TLA intervals were often even more localized than the ~300 km effective radius of GMDs: occurring at only some of the stations at which GMDs occurred. We show that TLA-related GMD events can result from dipolarization fronts in the magnetotail and fast flows toward Earth and are closely temporally associated to poleward boundary intensifications (PBI) and auroral streamers. The highly localized behavior and connection to the most extreme GMD events suggests that TLA intervals are a ground manifestation of the features within rapid and complex ionospheric structures that can drive GICs.
Creator
Depositor
  • bmccuen@umich.edu
Contact information
Discipline
Funding agency
  • National Aeronautics and Space Administration (NASA)
  • National Science Foundation (NSF)
ORSP grant number
  • 2013433, 1848724, 80NSSC20K1779
Keyword
Citations to related material
  • McCuen, B. A., Moldwin, M. B., Engebretson, M. J., Weygand, J. G., Nishimura, Y. (2023). A Statistical Analysis of High-frequency Transient-Large-Amplitude Geomagnetic Disturbance. [To be submitted to] Journal of Geophysical Research: Space Physics
Related items in Deep Blue Documents
Resource type
Curation notes
  • On 7 June 2023, the prod_initDepreciated.zip folder was deprecated and a new prod_init.zip folder was added. The deprecated folder has an error in the code of the script "get_onset_delays_withdiff.py" within the /prod_initDepreciated/init_tools/ folder. The new /prod_init.zip folder now includes the script titled "get_onset_info.py" in the /prod_init/init_tools/ folder, as well as the folder /Vsw_lists/ consisting of lists of solar wind flow speed data and two additional python scripts titled 'analysis_init_od.py' and 'analysis_init_ascii.py'. The folder 'TLA Substorms' was also added to include lists of substorms that have associated TLA intervals within 30 minutes. These corrections and additions are prompted by referee reviews to the original manuscript.

  • On 25 August 2023, the prod_allyra_allstns.txt file was deprecated and a new version of the file was added. This was due to incorrect MLT values in the deprecated file. The readme was deprecated and an updated version was added. Also, a new file TLAEvents_allyrs_allstns.txt was added. These corrections and additions were prompted by the data set creators finding mistakes.
Last modified
  • 08/25/2023
Published
  • 04/07/2023
Language
DOI
  • https://doi.org/10.7302/9par-f788
License
To Cite this Work:
McCuen, B. A. (2023). A Statistical Analysis of High-frequency Transient-Large-Amplitude Geomagnetic Disturbances: Data [Data set], University of Michigan - Deep Blue Data. https://doi.org/10.7302/9par-f788

Relationships

This work is not a member of any user collections.

Files (Count: 22; Size: 200 MB)

Date: 14 June, 2023

Dataset Title:
A Statistical Analysis of High-frequency Transient-Large-Amplitude Geomagnetic
Disturbances: Data

Dataset Creators:
McCuen, Brett A.

Dataset Contact:
bmccuen@umich.edu

Funding:
National Science Foundation (NSF)
National Aeronautics and Space Administration (NASA)

Abstract:
We present a comprehensive statistical analysis of high-frequency transient-large-amplitude
(TLA) magnetic perturbation events that occurred at 12 high-latitude ground magnetometer
stations throughout solar cycle 24 from 2009 to 2019. TLA signatures are defined as one or
more second-timescale dB/dt interval with magnitude ≥ 6 nT/s within
an hour event window. This study characterizes high-frequency TLA events based on their spatial
and temporal behavior as well as relation to auroral substorms, geomagnetic storm phases and
nighttime geomagnetic disturbance events events (GMD). We show that TLA events occur primarily
at nighttime and solely in the high-latitude region above 60 degrees geomagnetic latitude. The
largest TLA events occurred more often in the declining phase of the solar cycle when solar
wind velocity was higher and ring current activity was lower, suggesting association to
high-speed flows caused by coronal holes and subsequent corotating interaction regions reaching
Earth. TLA perturbations often occurred preceding or within the most extreme nighttime
geomagnetic disturbance (GMD) events with 5-10 minute timescales, but the TLA intervals were
often even more localized than the ~300 km effective radius of GMDs:
occurring at only some of the stations at which GMDs occurred. We show that TLA-related GMD
events can result from dipolarization fronts in the magnetotail and fast flows toward Earth
and are closely temporally associated to poleward boundary intensifications (PBI) and auroral
streamers. The highly localized behavior and connection to the most extreme GMD events suggests
that TLA intervals are a ground manifestation of the features within rapid and complex
ionospheric structures that can drive GICs.

--------------------------------------------------------------------------------------------------
Methodology:

The data in this repository are transient-large-amplitude dB/dt intervals with second-timescale
and amplitude > 6 nT/s. These dB/dt intervals are identified by the automated geomagnetic
disturbance classifier described in detail in McCuen et al. (2023). This automated technique is
run on yearly data files from individual magnetometer stations and saves the data product files
that are in the filepath: 'prod_init/Products/"year"/' and have the filename structure:
'"station code"/"year"/_algfinal_2-60s_6-1000nT_6-100nTs_xyz_filterf_svmvote_chk.csv'.
The data within these files is structured with the columns: ['start time', 'end time',
'start B value', 'end B value', 'dB (change in magnetic field strength)',
'dt (change in seconds)', 'dbdt (change in B divided by change in seconds)', 'component',
'station code']. These data product files are created for a set of stations from five
magnetometer arrays, the details of which are described in the instruments section below.
All available data from these stations from the years of 2009 to 2019 were used and the data
products saved in the yearly folders located at the filepath mentioned above.

*Note that the terms nighttime magnetic perturbation event (MPE) and geomagnetic disturbance
event (GMD) are used interchangeably in this document and in the relative python scripts and data
file names.
--------------------------------------------------------------------------------------------------
Files contained:

/prod_init/ folder:
- - - - - - - - - - - - - - - - - - -
*Note that the '/init_tools/' folder has an empty '__init__.py' script that is required for
the package to be used in the analysis_init.py and mpe_init.py scripts

analysis_init.py
From each station and each year of data product files in the filepaths
'prod_init/Products/"year"/', analysis_init.py will load each file and create 11 dataframes,
one for each year 2009-2019 with the load_products() function. For each yearly dataframe, the
following functions are performed:

/prod_init/init_tools/mlts.py contains get_mlts() which returns the magnetic local start and
end time of each dB/dt interval
/prod_init/init_tools/get_onset_delays_withdiff.py contains get_onset_delays_withdiff() which
uses the substorm event lists from
'/prod_init/Substorm Lists/' and then
returns the time delay from the most recent substorm onset for
each interval.
/prod_init/init_tools/get_smes.py contains get_smes() which uses the SME lists from
'/prod_init/SME Lists/' and then
returns the SuperMAG Electrojet Index (SME) for the
corresponding starting minute of each interval
/prod_init/init_tools/get_smrs.py contains get_smrs() which uses the SMR lists from the path
'/prod_init/SMR Lists/' and then
returns the SuperMAG Ring Current Index (SMR) for the
corresponding starting minute of each interval
These columns are then added to the main data product dataframe (column titles and descriptions
listed above in Methodology section) and saved as
'Products/'+'prod_allyrs_allstns_onstdiff_sme_smr.csv'. The added columns are:
'mlt_st' and 'mlt_et' = local magnetic start and end time
'onset_delay' = time delay from the most recent substorm onset
'sme' = SuperMAG electrojet index during the starting minute of the interval
'smr' = SuperMAG electrojet index during the starting minute of the interval

analysis_init_od.py
This script is similar to analysis_init.py with a few distinctions.
From each station and each year of data product files in the filepaths
'prod_init/Products/"year"/', analysis_init.py will load each file and create 11 dataframes,
one for each year 2009-2019 with the load_products() function. For each yearly dataframe, the
following functions are performed:

/prod_init/init_tools/mlts.py contains get_mlts() which returns the magnetic local start and
end time of each dB/dt interval
/prod_init/init_tools/get_onset_info.py contains get_onset_info() which
uses the substorm event lists from
'/prod_init/Substorm Lists/' and then
returns the time delay from the most recent substorm onset for
each interval, as well as the magnetic local time of the onset
delay of the substorm onsets and the latitude and longitude of the
substorm onset.

These columns are then added to the main data product dataframe (column titles and descriptions
listed above in Methodology section) and saved as
'Products/'+'prod_allyrs_allstns_od.csv'.
The added columns are:
'mlt_st' and 'mlt_et' = local magnetic start and end time
'onset_delay' = time delay from the most recent substorm onset
'od_mlt' = magnetic local time of substorm onset
'od_lat' = geographic latitude of substorm onset
'od_lon' = geographic longitude of substorm onset

analysis_init_ascii.py
This file loads the data product .csv files and creates a .txt file of all of the TLA interval
data.
From each station and each year of data product files in the filepaths
'prod_init/Products/"year"/', analysis_init.py will load each file and create 11 dataframes,
one for each year 2009-2019 with the load_products() function. For each yearly dataframe, the
following functions are performed:

/prod_init/init_tools/mlts.py contains get_mlts() which returns the magnetic local start and
end time of each dB/dt interval
These columns are then added to the main data product dataframe (column titles and descriptions
listed above in Methodology section) and saved as 'prod_allyrs_allstns.txt'.
The added columns are:
'mlt_st' = local magnetic start time
This file also has some formatting differences to remove any instances of string characters so
that the data columns have only numbers. The component values in the 'comp' columns are:
'1' = x
'2' = y
'3' = z
The station locations are in number codes instead of letter codes:
'igl' = 1
'gjo' = 2
'rby' = 3
'cdr' = 4
'pgg' = 5
'rank' = 6
'ykc' = 7
'fcc' = 8
'gill' = 9
'whit' = 10
'atha' = 11
'mea' = 12

mpe_init.py
This file loads MPE text files from the path '/MPE Derivs GE 6/' (data in Deep
Blue https://doi.org/10.7302/275e-da06) for the CDR, RBY, PGG stations
for 2015-2019, then performs the following functions:

/prod_init/init_tools/mpe_mlts.py contains get_mlts() which returns the magnetic local start and
end time of each dB/dt interval for the MPES
get_onset_delays_withdiff.py (see above)
get_smes() (see above)
get_smrs() (see above)

These columns are then added to the main data product dataframe and saved as
'Products/'+'mpes_onstdiff_sme_smr.csv'. The columns of this file are:
'st' = start time of the MPE
'station' = station where MPE occurred
'mpe_maxdbdt' = max dB/dt value of the MPE
'mlt_st', 'onset_delay', 'sme', 'smr' = same as described above

These three files:
'prod_allyrs_allstns_onstdiff_sme_smr.csv'
'mpes_onstdiff_sme_smr.csv'
'prod_allyrs_allstns_od.csv'
are the general data files for which all data analysis is based on. All statistics and subsets
of data are created from the data in these two data files.

Two other TLA data files were created manually from the main TLA data file:
'prod_allmlat_unrelated.csv' : which consists of all of the 'unrelated' events from 2015-2019
'prod_allmlat_maxes.csv' which consists of the maximum dB/dt of each event from 2015-2019, this
file has two additional columns:
'abs_dbdt' = absolute value of the dB/dt for each interval
'storm_phase' = the geomagnetic storm phase in which the event occurred. If the event did not
occur in relation to a geomagnetic storm, the value is '-'

tla_analysis.py script:
- - - - - - - - - - - - - - - - - - -
This python script loads the full data product file 'prod_allyrs_allstns_onstdiff_sme_smr.csv'
that was created via the analysis_init.py script as well as the file
'prod_allmlat_unrelated.csv' that contains data products for the years of 2015-2019 that are
termed unrelated because they occur more than 60 minutes from substorm onset and in the
absence of a geomagnetic storm phase. This file contains a subset of events form the file
'prod_allyrs_allstns_onstdiff_sme_smr.csv' and was created manually.

Then uses functions from the file
'/tools/analysis_tools.py' to create figures for the manuscript. These are described below:
*Note that the '/tools/' folder has an empty '__init__.py' script that is required for
the package to be used in the analysis_init.py and mpe_init.py scripts

sep_fullyrs(prod_allyrs): this function takes the full data set file and separates it in to the
stations that have available data for all years from 2009-2019 (see Supporting Information
Table S1) and returns the 'prod_fullcycle' dataframe
plot_num_vs_year_vsw_smr(prod_fullcycle): function takes the prod_fullcycle dataframe and
creates a plot of the number of extreme (>12 nT/s) events per year as a function of the SMR
value and the solar wind flow velocity.
plot_num_vs_year_multi(prod_fullcycle): function takes the prod_fullcycle dataframe and plots
the normalized number of TLA events per year as well as the number of substorm onsets, mean
sunspot number and number of extreme TLA events per year

sep_fullmlat(prod_allyrs): this function takes the full data set file and separates it in to
the stations that have available data for all years from 2015-2019 (see Supporting Information
Table S1) and returns the 'prod_allmlat' dataframe
sep_mlats(prod_mrge): takes the prod_mrge dataframe that is the prod_allyrs dataframe merged with
the prod_unrel dataframe so that there is an indicator of which events are'unrelated' and
separates this dataframe into four separate regions of magnetic latitude
plot_maxdbdt_nums_vs_mlt(prod_high, prod_midhigh, prod_midlow, prod_low): takes the four mlat
region dataframes and creates plots for the maximum dB/dt vs. MLT and the number of events vs. MLT
plot_dbdt_vs_sme_smr(prod_high, prod_midhigh, prod_midlow, prod_low): takes the four mlat region
dataframes and creates plots for the maxmimum dB/dt vs. SME and maximum dB/dt vs. SMR

mpe_plot_v4.py script:
- - - - - - - - - - - - - - - - - - -
This script loads the MPE data files from 2015-2019 for CDR, RBY, and PGG similarly to the
mpe_init.py file but with a slightly different format to include TLA dB/dt information in the
dataframe. Then there are two functions for plotting:
plot_(prod): plots the max dB/dt of each MPE-related TLA event as a function of the time
difference from the maximum dB/dt of the nearest MPE event

mpe_tla_compare.py script:
- - - - - - - - - - - - - - - - - - -
This script loads the TLA max dB/dt file 'prod_allmlat_maxes.csv and the MPE data file
'mpes_onstdiff_sme_smr.csv', then uses the following functions
get_mpe_diff(prod, mpe): finds the minimum time difference of each MPE event to the nearest TLA
event, the station that the TLA event occurred and the max dB/dt value of the TLA event, these
are then added to the MPE dataframe
spatial_scales(prod): which takes in the MPE dataframe and plots the number of stations at which
an event occurred based on how many stations the TLA event was identified at
mpe_rel_histos(): plots the percent of total MPE events that had TLA intervals and did not have
TLA intervals as a function of the maximum dB/d range of the events.

plot_09302016.py script:
- - - - - - - - - - - - - - - - - - -
This script uses the following functions to plot magnetic field data and TLA intervals.
get_thm_data(station, year, month, day): downloads data from the THEMIS database for the station
and data specific as the function arguments, then returns the data as a dataframe
get_maccs_data(station, year, month, day): downloads data from the MACCS database for the station
and data specific as the function arguments, then returns the data as a dataframe
get_prod(prod, station, date): takes the prod_allyears dataframe loaded from the
'prod_allyrs_allstns_onstdiff_sme_smr.csv' file and identifies the specific TLA intervals that
correspond to the station and date
avg_prod( prod, data, start, duration): calculates the average magnetic field data B value for
the interval specified by start and duration and substracts it from the start and end B value of
the TLA intervals of the product
avg_data(data, start, duration): calculates the average magnetic field data B value for the
interval specified by start and duration and subtracts from each data value
avg_data2(data, start, duration): performs same function as avg_data but for a 1-sec measurement
frequency rather than 1/2 second

plot_goesdata_09302016.py script:
- - - - - - - - - - - - - - - - - - -
This script takes magnetic field data and plots it. The data is downloaded manually from the
GOES-13 database (https://satdat.ngdc.noaa.gov/sem/goes/data/full/),
the specific data file is included in the repository as filename
'g13_magneto_512ms_20160930_20160930.csv'

tla_analysis_v3.py script:
- - - - - - - - - - - - - - - - - - -
This python script loads the full data product file 'prod_allyrs_allstns_onstdiff_sme_smr.csv'
that was created via the analysis_init.py script and performs some functions to create the plots
included in the publication
plot_daily_rates(prod): creates a plot of the number of TLA events per day from the 'prod'
dataframe with the number of substorms per day from the substorm event lists in the
'/prod_init/Substorm Lists/' folder
mlt_lat_od_pdf(prod): plots histograms of the distribution of events for the magnetic local time
at which the max dB/dt of the event occurred and the distribution of events for the magnetic
latitude at which the event occurred
get_vsw(prod): returns a dataframe of the max dB/dt of each event that includes a column of
the solar wind flow speed, Vsw, for the minute of the max dB/dt for each event. The Vsw values
are read from the lists located in '/prod_init/Vsw Lists/'.
vsw_smr_pdf(): creates histograms of the total SuperMAG Ring current values (SMR) for 2009-2019
with the SMR values at the minute of the max dB/dt of each event, as well as the total Vsw
values for 2009-2019 and the Vsw during the max dB/dt of each event

plot_od_londiff.py script:
- - - - - - - - - - - - - - - - - - -
This script loads the TLA max dB/dt file 'prod_allyrs_allstns_od.csv' and the MPE data file
'mpes_onstdiff_sme_smr.csv', then uses the following functions:
get_allmlat_od_maxes(): loads the 'prod_allyrs_allstns_od.csv' and returns a subset of events
from 2015-2019 with only the max dB/dt of each event
od_londiff(prod_max, ms_df, ms_df_ext): creates distributions of the number of events for the
time delay from substorm onset and for the difference in longitude from substorm onset for each
event with color separation for the GMD-related events

/TLA Substorms/ folder:
- - - - - - - - - - - - - - - - - - -
This folder contains the script 'get_substorms.py' that locates the substorms that have TLA intervals
within 30 minutes of the time of substorm onset and saves this list of TLA related substorm onsets in
the same folder. These lists have the filenames:
'TLA_substorms-newell-'+year+'0101_000000_to_'+year+'1231_000000.csv'
for each year from 2009-2019

--------------------------------------------------------------------------------------------------
Instrument and/or Software specifications:

This database used data products created using magnetic field data from five magnetometer arrays.
The details of these programs and their instrumentation is listed below.

1) The Magnetometer Array for Cusp and Cleft Studies (MACCS) is a system of magnetometers
located in north-east Nunavut, Canada from about 65° to 80° geomagnetic latitude
(Engebretson, 1995) MACCS is operated by Augsburg University and the University of Michigan and
is funded by the National Science Foundation (NSF). The MACCS stations contain fluxgate
magnetometers with axes aligned with the Earth's magnetic field (H: magnetic north-south, D:
east-west, Z: vertical with positive direction downward into Earth). The MACCS magnetometers
measure the magnetic field at 8 Hz and then average and record the measurements at 2 Hz
(half-second cadence). This results in temporal resolution of 0.025 nT and the measurements are
accurate to 0.01 nT.
MACCS stations used are: IGL, GJO, RBY, PGG, CDR

2) The Canadian Array for Realtime InvestigationS of Magnetic Activity (CARISMA) is a system of
ground-based magnetometers located across central Canada (Mann, 2008). CARISMA is operated by
the University of Alberta as part of the Canadian Geospace Monitoring Program (CGSM) and is
funded by the Canadian Space Agency (CSA). Like MACCS, the CARISMA system consists of fluxgate
magnetometers that measure the magnetic field at 8 samples/second. The stations used in this study
offer final data products that are averaged to 2 samples/s and rotated from the geographic
coordinates they are originally measured in to local geomagnetic coordinates. These magnetometer
systems offer 0.025 nT resolution data.
CARISMA stations used are: GILL, ATHA

3) The the CANadian Magnetic Observatory System (CANMOS) (Nikitina, 2016) is a ground magnetometer
array operated by Natural Resources Canada (NRCan). CANMOS employs fluxgate magnetometers across
Canada that sample the magnetic field at 8 Hz, then resamples to 1 Hz after despiking and
performing a 9-point rectangular filter. The data from CANMOS is in geographic coordinates:
X (geographic north-south), Y (geographic east-west) and Z (vertical).
CANMOS station used are: YKC, FCC, MEA

4) The Athabasca University Time History of Events and Macroscale Interactions During Substorms
(THEMIS) University of California, Los Angeles (UCLA) Magnetometer Network eXtension (AUTUMNX)
(Connors, 2016) is located in the eastern region of Canada. The AUTUMNX instruments are fluxgate
magnetometers provided by UCLA that measure the magnetic field with 0.01 nT resolution at
2 samples/second and in local geomagnetic coordinates.
AUTUMNX stations used are: SALU, KJPK

5) THEMIS Ground-Based Observatory (GBO) systems (Russell, 2008) are a part of the larger
collaboration of stations that contribute magnetic data to the THEMIS Ground Magnetometer (GMAG)
cooperative. THEMIS GBO stations are operated by UCLA, contain UCLA instruments as in (4) and
thus have the same resolution, measurement frequency and coordinate system as mentioned above.
THEMIS GBO stations used are: WHIT

--------------------------------------------------------------------------------------------------
References:

Connors, M., Schofield, I., Reiter, K., Chi, P. J., Rowe, K. M., & Russell, C. T. (2016). The
AUTUMNX magnetometer meridian chain in Québec, Canada. Earth, Planets and Space, 68(1).
https://doi.org/10.1186/s40623-015-0354-4

Engebretson, M. J., Hughes, W. J., Alford, J. L., Zesta, E., Cahill, L. J., Arnoldy, R. L., &
Reeves, G. D. (1995). Magnetometer array for cusp and cleft studies observations of the spatial
extent of broadband ULF magnetic pulsations at cusp/cleft latitudes. Journal of Geophysical
Research, 100(A10), 19371. https://doi.org/10.1029/95ja00768

Mann, I. R., Milling, D. K., Rae, I. J., Ozeke, L. G., Kale, A., Kale, Z. C., Murphy, K. R.,
Parent, A., Usanova, M., Pahud, D. M., Lee, E.-A., Wallis, D. D., Angelopoulos, V.,
Glassmeier K.-H., Russell, C. T., Auster, H.-U., Singer, H. J. (2008). The upgraded CARISMA
magnetometer array in the THEMIS era. Space Science Reviews, 141(1–4), 413–451.
https://doi.org/10.1007/s11214-008-9457-6

McCuen, B. A., Moldwin, M. B., Steinmetz, E. S., & Engebretson, M. J. (2023). Automated
High-Frequency Geomagnetic Disturbance Classifier: A Machine Learning Approach to Identifying
Noise While Retaining High-Frequency Components of the Geomagnetic Field. Journal of Geophysical
Research: Space Physics, 128(2). https://doi.org/10.1029/2022JA030842

Nikitina, L., Trichtchenko, L., & Boteler, D. H. (2016). Assessment of extreme values in
geomagnetic and geoelectric field variations for Canada. Space Weather, Vol. 14, pp. 481–494.
https://doi.org/10.1002/2016SW001386

Russell, C. T., Chi, P. J., Dearborn, D. J., Ge, Y. S., Kuo-Tiong, B., Means, J. D., … Snare, R.
C. (2008). THEMIS ground-based magnetometers. Space Science Reviews, 141(1–4), 389–412.
https://doi.org/10.1007/s11214-008-9337-0

Curation Notes:
On 7 June 2023, the prod_initDepreciated.zip folder was deprecated and a new prod_init.zip folder was
added. The deprecated folder has an error in the code of the script "get_onset_delays_withdiff.py"
within the /prod_initDepreciated/init_tools/ folder. The new /prod_init.zip folder now includes the
script titled "get_onset_info.py" in the /prod_init/init_tools/ folder, as well as the folder
/Vsw_lists/ consisting of lists of solar wind flow speed data and two additional python scripts
titled 'analysis_init_od.py' and 'analysis_init_ascii.py'. The folder 'TLA Substorms' was also added
to include lists of substorms that have associated TLA intervals within 30 minutes.
These corrections and additions are prompted by referee reviews to the original manuscript.

On June 14, 2023 the movie file titled "thg_asi_mosaic_201609300100kuuj.mpeg" was added. This is a
mosaic composition of images from THEMIS all-sky imagers (ASI) at four stations for an hour interval
on September 30, 2016.

Download All Files (To download individual files, select them in the “Files” panel above)

Best for data sets < 3 GB. Downloads all files plus metadata into a zip file.

Files are ready   Download Data from Globus
Best for data sets > 3 GB. Globus is the platform Deep Blue Data uses to make large data sets available.   More about Globus

Remediation of Harmful Language

The University of Michigan Library aims to describe library materials in a way that respects the people and communities who create, use, and are represented in our collections. Report harmful or offensive language in catalog records, finding aids, or elsewhere in our collections anonymously through our metadata feedback form. More information at Remediation of Harmful Language.