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Ice wedges are widespread periglacial features in the landscape of Adventdalen, Svalbard. The networks of ice wedges have created areas with well-developed polygonal terrains in the lowest fluvial ter...
Results from a study of benthic nitrogen cycling in two Arctic fjords are presented. Intact sediment core incubations were used to quantify net fluxes of dissolved inorganic nitrogen, organic nitroge...
This paper reports on backscatter and depolarization measurements by an airborne lidar in the Arctic during the ASTAR 2004 campaign. A unique weather situation facilitated the observation of the aeros...
The dynamics and mass balance regime of the Austfonna ice cap, the largest glacier on Svalbard, deviates significantly from most other glaciers in the region and is not fully understood. We have compa...
The observed rapid climate warming in the Arctic requires improvements in permafrost and carbon cycle monitoring, accomplished by setting up long-term observation sites with high-quality in-situ measu...
A new discovery of ornithopod dinosaur tracks from Svalbard is described. The Lower Cretaceous (Barremian) section at Isfjorden consists of sandstones and interbeds consistent with an alluvial flood p...
Travertines from the Troll thermal springs,Svalbard     Travertines  Troll thermal springs  Svalbard       font style='font-size:12px;'> 2009/12/3
The Troll and Jotun hot springs are located along the Bockfjorden fault zone at 79°23’N on Svalbard and represent the northernmost thermal springs documented on land. They are recharged through subper...
Thirty-six seabed samples from inshore and offshore Svalbard and the northern part of the Barents Sea were collected for dinoflagellate cyst (dinocyst) analysis. Svalbard is an important locality repr...
We present steady state (diagnostic) and transient (prognostic) simulations of Midtre Lovénbreen, Svalbard performed with the thermo-mechanically coupled full-Stokes code Elmer. This glacier has an ex...
Subpermafrost Groundwater,Western Svalbard      Subpermafrost Groundwater  Western Svalbard        font style='font-size:12px;'> 2009/10/26
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       font style='font-size:12px;'> 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...
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        font style='font-size:12px;'> 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...
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...
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 ...

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