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Recent Northern Hemisphere snow cover extent trends and implications for the snow‐albedo feedback
Author(s) -
Déry Stephen J.,
Brown Ross D.
Publication year - 2007
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2007gl031474
Subject(s) - northern hemisphere , albedo (alchemy) , climatology , snow , snow line , latitude , snow cover , spring (device) , anomaly (physics) , environmental science , physical geography , geology , geography , mechanical engineering , art , physics , geodesy , condensed matter physics , geomorphology , performance art , engineering , art history
Monotonic trend analysis of Northern Hemisphere snow cover extent (SCE) over the period 1972–2006 with the Mann‐Kendall 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 −1.28, −0.78, and −0.48 × 10 6 km 2 (35 years) −1 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‐albedo feedback over northern latitudes that acts to reinforce an initial anomaly in the cryospheric system.