Study of the Characteristics of the Supraglacial Runoff of the Austre Grønfjordbreen, Spitsbergenстатья
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Аннотация:This article considers the characteristics of two systems of the supraglacial runoff of the polar gla-
cier: a hydro-network of streams and a porous layer of melting crust. Field methods have revealed fundamen-
tal differences between these systems in the drainage area and the features of the meltwater movement and
runoff regime. Calculation of the supraglacial runoff has shown its maximum level in the hydro-network
during the peak of snowmelt in July, while the runoff in the melting crust becomes predominant in the second
half of summer (in August).