Тепловыделение при метаморфических процессах в снежном покрове

Abstract

The work analyzes known metamorphic processes in the snow from the point of view of the energy approach. A list of these processes supplemented by processes associated with the run-off quasi-liquid layer of snow granules. Experimental results on the heat of the volume of snow and the temperature gradient in the depth of the snow cover. It was stressed that the snow is not just a passive conductor of heat, but it is also heat-emitting.