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Preferential Flow and Melt Water Retention in Cold Snow Packs in West-Greenland
Preferential Flow Melt Water Retention Cold Snow Packs West-Greenland
2009/10/23
Runoff from seasonal snow covers in Greenland provides the major source of
stream flow in the non-glacierized catchments, and has gained interest in relation
to hydropower potentials and water suppl...
Snow-Distribution Modelling in the Ammassalik Region,South East Greenland
Snow-Distribution Modelling Ammassalik Region South East Greenland
2009/10/22
The Ammassalik region is characterized by a strong alpine relief, with altitudes
up to 1,000 m. Glaciers are located mainly on the western side of ridges. The climate
is low arctic, with annual prec...