Snow Cover

نویسنده

  • Kotlyakov Vladimir
چکیده

Snow cover is a layer of snow on the earth’s surface, which is mainly results from snowfalls. The snow cover can be temporary, when a snow melts during several hours or days after its formation, and it can be stable, when it remains for the whole winter or with short interruptions. The snow cover formation on the globe is determined (conditioned) by the geographical zonality, surface relief, and general circulation of the atmosphere. Solid precipitation is a source of snow cover; it remains on the earth surface at negative temperatures. Wind-blown snow transport results in sharp irregularity of its deposition, especially in mountains.

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تاریخ انتشار 2011