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Recent Trends In Laurentian Great Lakes Ice Cover

dc.contributor.authorAssel, Raymonden_US
dc.contributor.authorCronk, Kevinen_US
dc.contributor.authorNorton, Daviden_US
dc.date.accessioned2006-09-08T20:29:40Z
dc.date.available2006-09-08T20:29:40Z
dc.date.issued2003-03en_US
dc.identifier.citationAssel, Raymond; Cronk, Kevin; Norton, David; (2003). "Recent Trends In Laurentian Great Lakes Ice Cover." Climatic Change 57 (1-2): 185-204. <http://hdl.handle.net/2027.42/42580>en_US
dc.identifier.issn0165-0009en_US
dc.identifier.issn1573-1480en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/42580
dc.description.abstractA 39-winter (1963–2001) record of annual maximum ice concentration (AMIC), the maximum fraction of lake surface area covered by ice each year, is analyzed for each Great Lake. Lake Erie has the largest median AMIC (94%) followed by Lakes Superior (80%), Huron(63%), Michigan (33%), and Ontario (21%). The frequency distributionof AMICs is negatively skewed for Lakes Superior and Erie and positively skewed for Lakes Michigan and Ontario. Temporal and spatial patterns of typical and extreme AMICs is presented within the context of long-term average air temperatures and lake bathymetry. The variation of spatially averaged ice concentration with discrete depth ranges are discussed for each lake for the upper and lower end of the typical range of AMIC values. In general, ice concentration decreases with increasing depth ranges for a given winter. A decrease in the gradient of ice concentration with depths was also observed with an increase in the AMIC from winter 1983 to winter 1984. A temporal trend in the AMICs supports the hypothesis of three ice cover regimes over the past 39 winters. Approximately 44% of the highest quartile (10 highest) AMICs for the Great Lakes occurred during the 6-winter period:1977–1982 providing evidence of a higher ice cover regime during thisperiod relative to the 14 winters before them (1963–1976) and the 19 winters after them (1983–2001). Winter 1998 established new low AMIC extremes,and the AMIC averaged over the 1998–2001 winters is the lowest for theperiod of record on four of the five Great Lakes. These recent trends taken together are noteworthy as they may be harbingers of a period of even lower AMICs in the 21st Century.en_US
dc.format.extent250691 bytes
dc.format.extent3115 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherKluwer Academic Publishers; Springer Science+Business Mediaen_US
dc.subject.otherGeosciencesen_US
dc.subject.otherMeteorology/Climatologyen_US
dc.titleRecent Trends In Laurentian Great Lakes Ice Coveren_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelEcology and Evolutionary Biologyen_US
dc.subject.hlbsecondlevelAtmospheric, Oceanic and Space Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumCooperative Institute for Limnology and Ecosystems Research, The University of Michigan, 2200 Bonisteel Boulevard, Ann Arbor, Michigan, 48109-2099, U.S.Aen_US
dc.contributor.affiliationotherNational Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory, 2205 Commonwealth Blvd, Ann Arbor, Michigan, 48105-2945, U.S.Aen_US
dc.contributor.affiliationotherNational Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory, 2205 Commonwealth Blvd, Ann Arbor, Michigan, 48105-2945, U.S.Aen_US
dc.contributor.affiliationumcampusAnn Arboren_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/42580/1/10584_2004_Article_5095423.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1023/A:1022140604052en_US
dc.identifier.sourceClimatic Changeen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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