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The hydrological studies of the Greenland technical Organization in Greenland
are being followed up at Copenhagen by hydrological data work as well
as hydrological model-simulation.
The hydrologica...
Hydrological Background of a Glacier-Influenced Hydropower Station in Greenland
Hydrological Background Glacier-Influenced Hydropower Station Greenland
2009/10/27
For planning a hydropower station at Paakitsup Akuliarusersua in West Greenland,
some unusual hydrological studies were required. The basin is situated
about 45 km north-east of Ilulissat/Jakobshavn...
Application of Satellite Data to Monitoring Snow Cover and Runoff in Greenland
Satellite Data Snow Cover Runoff Greenland
2009/10/27
Based on NOAA-AVHRR satellite data and runoff records from one of the
major drainage basins in Western Greenland methods for monitoring snow
cover, snowpack water equivalent and runoff have been ela...
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...
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...