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Integrated water vapor above Ny Ålesund, Spitsbergen: a multi-sensor intercomparison
Integrated water vapor Ny Å lesund Spitsbergen multi-sensor intercomparison
2010/2/21
Water vapor is an important constituent of the atmosphere. Because of its abundance and its radiative properties it plays an important role for the radiation budget of the atmosphere and has major inf...
Cluster analysis of the impact of air back-trajectories on aerosol optical properties at Hornsund, Spitsbergen
air back-trajectories aerosol optical properties Hornsund Spitsbergen
2010/2/1
In this paper, spectra of aerosol optical thickness from the AERONET (AErosol RObotic NETwork) station at Hornsund in the southern part of Spitsbergen were employed to study the impact of air mass his...
Tertiary structure of the Sørkapp-Hornsund Region,South Spitsbergen,and implications for the offshore southern extension of the fold-thrust Belt
Tertiary structure Sø rkapp-Hornsund Region offshore southern extension fold-thrust Belt
2009/12/3
The Sørkapp-Hornsund region of southern Spitsbergen has undergone a complex Tertiary tectonic history, including contractional and transpressional uplift and transtensional subsidence and react...
Paralic sedimentation on an epicontinental ramp shelf during a full cycle of relative sea-level fluctuation;the Helvetiafjellet Formation in Nordenskiöld land,Spitsbergen
Paralic sedimentation epicontinental ramp shelf full cycle relative sea-level fluctuation
2009/12/2
A depositional model for the development of the Helvetiafjellet Formation in Nordenskiöld Land, Spitsbergen is presented. The formation was deposited into a segment of the large epicontinental Bo...
Lower Cretaceous lithostratigraphy across a regional subaerial unconformity in Spitsbergen:the Rurikfjellet and Helvetiafjellet formations
Lower Cretaceous lithostratigraphy regional subaerial unconformity Rurikfjellet and Helvetiafjellet formations
2009/12/2
During development of the Lower Cretaceous succession in the Spitsbergen domain of the epicontinental Boreal Basin, a fall in relative sea-level caused a major subaerial unconformity to form. This unc...
Swath bathymetry and high-resolution seismic data, as well as published material are used to analyse pockmarks in Spitsbergen fjords. Up to 250 m wide and 13 m deep pockmarks occur in Grønfjord...
The Hydrology of Bayelva,Spitsbergen
Hydrology Bayelva
2009/10/27
The hydrology of Bayelva, which is located to the northwestern part of Spitsbergen,
was investigated during the period 1974-78. The river drains a catchment
of 31.5 km2, out of which 54% are covered...
Hydrology of a Polythermal Glacier,Erikbreen,Northern Spitsbergen
Hydrology Polythermal Glacier
2009/10/26
Glacial and glaciohydrologic processes that control the glaciofluvial sediment
delivery from Erikbreen, a polythermal glacier on the north coast of Spitsbergen
(79"407N, 12"30'E), were studied durin...
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 ...
Mixing in the West Spitsbergen Current
West Spitsbergen Current Atlantic waters internal Rossby radius
2009/1/20
Twenty-eight profiles of temperature and salinity down to 1 km depth have been measured in the area north from the coast of Svalbard to latitude 84°40′N between 0 and 32°E longitude. They show Atlanti...