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Elevated erosion surfaces in central West Greenland and southern Norway:their significance in integrated studies of passive margin development
Elevated erosion surfaces southern Norway integrated studies passive margin development
2009/12/2
Elevated erosion surfaces were used as an independent data set in an integrated study of the landscape development in central West Greenland.The study resulted in a time-constrained model describing m...
Interpretation of the Positive-Degree-Days Factor by Heat Balance Characteristics–West Greenland
Positive-Degree-Days Factor Heat Balance Characteristics West Greenland
2009/10/27
From heat balance measurements in the ablation area of West Greenland
(EGIG-profile, 1,013 m a.s.l., 69"40'N, 49"38'W) the positive-degree-daysfactor
is interpreted by the heat balance characteristi...
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...
Partitioning of melt energy and meltwater fluxes in the ablation zone of the west Greenland ice sheet
melt energy meltwater fluxes ablation zone west Greenland ice sheet
2010/2/4
We present four years (August 2003–August 2007) of surface mass balance data from the ablation zone of the west Greenland ice sheet along the 67° N latitude circle. Sonic height rangers and automatic ...
Physical and chemical predictors of diatom dissolution in freshwater and saline lake sediments in North America and West Greenland
Physical and chemical predictors diatom dissolution in freshwater saline lake sediments North America West Greenland
2014/5/4
Diatom dissolution in surface sediment samples from two regional lake datasets in the Northern Great Plains (NGP; n = 64) and West Greenland (n = 40) is assessed using a morphological approach categor...