Sensitivity of Model-Generated Daytime Surface Heat Fluxes over Snow to Land-Cover Changes
Snow cover can significantly suppress daytime temperatures by increasing the surface albedo and limiting the surface temperature to 0°C. The strength of this effect is dependent upon how well the snow can cover, or mask, the underlying surface. In regions where tall vegetation protrudes through a sh...
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Published in | Journal of hydrometeorology Vol. 4; no. 1; pp. 24 - 42 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
American Meteorological Society
01.02.2003
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Online Access | Get full text |
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