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Subpmmafrost groundwater aquifers arc found in N~-Alesund, western Svalbard.
Recharge of groundwatcr takes place along thc basc of the nearby glaciers,
and groundwater tlows in open bedrock fracturc...
Subpermafrost Groundwater Modelling in Ny-Ålesund,Svalbard
Subpermafrost Groundwater Ny-Å lesund
2009/10/23
Svalbard is a high arctic archipelago where the permafrost thickness is 150-450
m and almost continuous in ice-free areas. The model work was carried out in
N~-Alesundw, here the subpermafrost aquif...
Fluxes of Water and Energy from Three High Latitude Tundra Sites in Svalbard
Fluxes of Water Three High Latitude Tundra Sites Svalbard
2009/10/23
Measurements of the surface fluxes of radiation, heat and water vapour were
made at three tundra sites near N~-Alesund, Svalbard for the active seasons
(June to September) of 1995 and 1996. In 1995 ...
Snow Distribution at a High Arctic Site at Svalbard
Snow Distribution High Arctic Site Svalbard
2009/10/23
In the Arctic regions snow cover has a major influence on the environment both
in a hydrological and ecological context. Due to strong winds and open terrain
the snow is heavily redistributed and th...
An Energy Balance Based HBV- Model with Application to an Arctic Watershed on Svalbard,Spitsbergen
Energy Balance HBV- Model Arctic Watershed
2009/10/22
In several studies of snowmelt using the temperature index method from the original HBV-model, the model fails to predict the timing of the snowmelt and underestimates the intensities on occasions wit...
Regional Variations of Snow Accumulation on Spitsbergen,Svalbard,1997-99
Regional Variations Snow Accumulation Spitsbergen
2009/10/22
End-of-winter snow accumulation has been measured over large areas on Spitsbergen,
Svalbard, using Ground Penetrating Radar (GPR) in the years of 1997,
1998, and 1999. Measuring transects following ...
