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Recent Northern Hemisphere snow cover extent trends and implications for the snow‐albedo feedback

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Déry, Stephen J., Brown, Ross D.·2007·Geophysical Research Letters

Abstract

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.

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Metadata

Authors
Déry, S. J., & Brown, R. D.
Venue
Geophysical Research Letters
Published
2007-11
Volume
34
Issue
22
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2093429038
Cited by
412
References
0
FWCI
5.33
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Recent Northern Hemisphere snow cover extent trends and implications for the snow‐albedo feedback. https://app.cochat.ai/papers/10.1029/2007gl031474
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Déry, S. J., & Brown, R. D. (2007). Recent Northern Hemisphere snow cover extent trends and implications for the snow‐albedo feedback. Geophysical Research Letters. https://doi.org/10.1029/2007gl031474

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