Abstract
ABSTRACT The paper presents a method of determination of areal value of degree-day factor by plotting basin snowmelt against the degree-day multiplied by the area of snow cover; some studies regarding stability of this degree-day factor are also presented. The question of open patches inside the snow cover poses difficult problems in conceptual modelling of snowmelt runoff. Some ignore it, others measure snow cover patch by patch. The paper suggests some ways of reconciling these two approaches.
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