CAUSE AND EFFECT OF VARIATIONS IN WESTERN ARCTIC SNOW AND SEA ICE COVER

Recent decreases in snow and sea ice cover in the high northern latitudes are indicators of climate change. A radiative perturbation known as the “temperature-albedo feedback ” is expected as temperatures rise

Bibliographic Details
Main Authors: R. S. Stone, D. C. Douglas, G. I. Belchansky, S. D. Drobot, J. Harris
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Arctic
albedo
Climate change
Sea ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.498.6452
Description
Summary:Recent decreases in snow and sea ice cover in the high northern latitudes are indicators of climate change. A radiative perturbation known as the “temperature-albedo feedback ” is expected as temperatures rise

Similar Items