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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Bibliographic Details
Published inJournal of hydrometeorology Vol. 4; no. 1; pp. 24 - 42
Main Authors Strack, John E., Pielke, Roger A., Adegoke, Jimmy
Format Journal Article
LanguageEnglish
Published American Meteorological Society 01.02.2003
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