The extent and variability of seasonal snow cover are important
parameters in the climate system, due to their effects on energy
and moisture budgets, and because surface temperature is highly
dependent on snow cover. In turn, snow cover trends serve as key
indicators of climate change. Many distinct techniques have become
available to study snow-climate relationships. Satellites provided
the first capability for monitoring snow cover extent at
continental and hemispheric scales, and there have been rapid
advances in snow modeling physics to represent snow cover and snow
processes in Global Climate Models (GCMs). These advances have
changed the way we look at snow cover. The main goal of this book
is to provide a synthesis of the prevailing state of snow-climate
science that reflects this distinct perspective. This volume
provides an excellent synthesis for researchers and advanced
students.
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