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Regional characteristics of chemical constituents in surface snow, Arctic cryosphere
Surface snow observations were carried out on many glaciers in the Arctic. The observational sites were in Svalbard, Severnaya Zemlya, Greenland and arctic Canada. The seasonal variations of chemical constituents in snowfall remained in the surface snow on the central Greenland ice sheet where the effect of snowmelt was weak. Conversely, the chemical constituents in the snow layer changed with infiltra tion of melt water on the Svalbard glacier where strong snowmelt occurred, even in highdoi:10.15094/00002930 fatcat:hyt75rfugbdvrdsrg55kjlp27y