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Differential accumulation of snow on fields



Differential accumulation of snow on fields



Zemledelie (1): 35-37



Data are given in the form of correction coefficients on the effects of slope and exposure to wind on snow accumulation and the effects of tillage depth and methods on the snow-derived moisture contents of sandy, loamy and clayey soils on slopes of <0.3, 0.3-1.0, 1.0-2.0 and 2.0-3.0 degrees. Soil water content of the 3-4 cm layer decreased as slope increased and as tillage depth was reduced.

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