## Abstract A substantial decrease in snow cover extent (SCE) and snow depth over North America has been observed over the 1960β2000 period. One explanation for the changes in North American snow cover is a change in the frequency and/or intensity of snow ablation. This study uses a gridded dataset
Spatial variability and trends in observed snow depth over North America
β Scribed by Dyer, Jamie L.; Mote, Thomas L.
- Book ID
- 119669579
- Publisher
- American Geophysical Union
- Year
- 2006
- Tongue
- English
- Weight
- 782 KB
- Volume
- 33
- Category
- Article
- ISSN
- 1944-8007
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