{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,30]],"date-time":"2026-04-30T20:55:24Z","timestamp":1777582524954,"version":"3.51.4"},"reference-count":26,"publisher":"American Geophysical Union (AGU)","issue":"22","license":[{"start":{"date-parts":[[2007,11,27]],"date-time":"2007-11-27T00:00:00Z","timestamp":1196121600000},"content-version":"vor","delay-in-days":26,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Geophysical Research Letters"],"published-print":{"date-parts":[[2007,11]]},"abstract":"<jats:p>Monotonic trend analysis of Northern Hemisphere snow cover extent (SCE) over the period 1972\u20132006 with the Mann\u2010Kendall test reveals significant declines in SCE during spring over North America and Eurasia, with lesser declines during winter and some increases in fall SCE. The weekly mean trend attains \u22121.28, \u22120.78, and \u22120.48 \u00d7 10<jats:sup>6<\/jats:sup> km<jats:sup>2<\/jats:sup> (35 years)<jats:sup>\u22121<\/jats:sup> over the Northern Hemisphere, North America, and Eurasia, respectively. The standardized SCE time series vary and trend coherently over Eurasia and North America, with evidence of a poleward amplification of decreasing SCE trends during spring. Multiple linear regression analyses reveal a significant dependence of the retreat of the spring continental SCE on latitude and elevation. The poleward amplification is consistent with an enhanced snow\u2010albedo feedback over northern latitudes that acts to reinforce an initial anomaly in the cryospheric system.<\/jats:p>","DOI":"10.1029\/2007gl031474","type":"journal-article","created":{"date-parts":[[2007,11,26]],"date-time":"2007-11-26T21:02:36Z","timestamp":1196110956000},"source":"Crossref","is-referenced-by-count":311,"title":["Recent Northern Hemisphere snow cover extent trends and implications for the snow\u2010albedo feedback"],"prefix":"10.1029","volume":"34","author":[{"given":"Stephen J.","family":"D\u00e9ry","sequence":"first","affiliation":[{"name":"Environmental Science and Engineering Program University of Northern British Columbia  Prince George, British Columbia Canada"}]},{"given":"Ross D.","family":"Brown","sequence":"additional","affiliation":[{"name":"Section des Processus Climatiques Environnement Canada \u00e0 Ouranos  Montr\u00e9al, Quebec Canada"}]}],"member":"13","published-online":{"date-parts":[[2007,11,27]]},"reference":[{"key":"e_1_2_6_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.rse.2006.09.035"},{"key":"e_1_2_6_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/2005GL022845"},{"key":"e_1_2_6_4_1","doi-asserted-by":"publisher","DOI":"10.1175\/JCLI3440.1"},{"key":"e_1_2_6_5_1","doi-asserted-by":"publisher","DOI":"10.1029\/2005JD006173"},{"key":"e_1_2_6_6_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442-12.1.230"},{"key":"e_1_2_6_7_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.263.5144.198"},{"key":"e_1_2_6_8_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(1994)007<1633:COSCTA>2.0.CO;2"},{"key":"e_1_2_6_9_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(1992)005<1441:IVOWSC>2.0.CO;2"},{"key":"e_1_2_6_10_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(1993)006<1327:RVOSCA>2.0.CO;2"},{"key":"e_1_2_6_11_1","volume-title":"Rank Correlation Methods","author":"Kendall M. 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