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The snow cover on lakes of the Arctic Coastal Plain of Alaska, U.S.A.

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Shallow lakes cover >25% of Alaska's Arctic Coastal Plain. These remain frozen and snow-covered from October to June. The lake snow is thinner, denser, harder and has less water equivalent than snow on the surrounding tundra. Itcontains less depth hoar than land snow, yet paradoxically is subject to stronger temperature gradients. It also has fewer layers and these have been more strongly affected by wind. Dunes and drifts are better developed on lakes; they have wavelengths of 5-20 m, compared to <5 m on land. Because of these differences, lake snow has roughly half the thermal insulating capacity of land snow.The winter mass balance on lakes is also different because (1) some snow falls into the water before the lakes freeze, (2) some snow accumulates in drifts surrounding the lakes, and (3) prevailing winds lead to increased erosion and thinner snow on the eastern lake sides. Physical models that extrapolate land snow over lakes without appropriate adjustments for depth, density, distribution and thermal properties will under-predict ice thickness and winter heat losses.

Document Type: Research Article

DOI: http://dx.doi.org/10.3189/172756503781830539

Publication date: June 1, 2003

More about this publication?
  • The Journal of Glaciology is published six times per year. It accepts submissions from any discipline related to the study of snow and ice. All articles are peer reviewed. The Journal is included in the ISI Science Citation Index.
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