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contributor authorBaker, D. G.
contributor authorSkaggs, R. H.
contributor authorRuschy, D. L.
date accessioned2017-06-09T14:03:27Z
date available2017-06-09T14:03:27Z
date copyright1991/03/01
date issued1991
identifier issn0894-8763
identifier otherams-11664.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146917
description abstractThe mean daily albedo of snow cover over sod, alfalfa, and bare soil was obtained over the course of 19 winters. This period provided a wide range of snow depths (up to 61 cm), albedos (a maximum of 95%), and densities (from less than 40 to more than 350 kg m?3). The mean over-winter height of the sod was 4 to 6 cm, while the alfalfa ranged from 7 to 15 cm tall. It was found that the rate of increase of the albedo with increasing snow depth showed a marked decrease once the albedo reached about 70%. It was also found that the standard deviation of the albedos decreased appreciably once the albedo reached 70%. Accepting an albedo of 70% as indicating the depth sufficient to effectively mask the underlying surface, 5, 7.5, and 15 cm of snow over the bare soil, sod, and alfalfa were required, respectively, for the three surfaces.
publisherAmerican Meteorological Society
titleSnow Depth Required to Mask the Underlying Surface
typeJournal Paper
journal volume30
journal issue3
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1991)030<0387:SDRTMT>2.0.CO;2
journal fristpage387
journal lastpage392
treeJournal of Applied Meteorology:;1991:;volume( 030 ):;issue: 003
contenttypeFulltext


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