Equilibrium State of Jakobshavns Isbræ, West Greenland

Tidal Flexure of Jakobshavns Glacier, West Greenland

Bed topography of Jakobshavn Isbræ, Greenland, and Byrd Glacier, Antarctica

This paper presents the bed topography of Jakobshavn Isbræ, Greenland, and Byrd Glacier, Antarctica, derived from sounding these glaciers with high-sensitivity radars. To understand the processes causing the speed-up and retreat of outlet glaciers, and to enable the development of nextgeneration ice-sheet models, we need information on bed topography and basal conditions. To this end, we perfor...

Analysis of the Motion Behaviour of Jakobshavn Isbræ Glacier in Greenland by Monocular Image Sequence Analysis

Jakobshavn Isbræ on the west coast of Greenland is one of the fastest and most productive glaciers in the world. It has been moving with an average velocity of 20 meters per day over a long time, producing to total annual iceberg volume of 30 40 km. In recent years a dramatic retreat of the glacier front has been observed. At the same time, a significant increase of the moving velocity has been...

Population structure of West Greenland narwhals

The hypothesis that different populations of narwhals in the West Greenland area exist has been tested by different biomarkers (metal and organochlorine concentrations, stable isotopes and DNA). Samples of muscle, liver, kidney, blubber and skin tissues of narwhals from West Greenland have been analysed for heavy metals, organochlorines, stable isotopes and DNA. The obtained results of metal co...

Glacier, fjord, and seismic response to recent large calving events, Jakobshavn Isbræ, Greenland

[1] The recent loss of Jakobshavn Isbræ’s extensive floating ice tongue has been accompanied by a change in near terminus behavior. Calving currently occurs primarily in summer from a grounded terminus, involves the detachment and overturning of several icebergs within 30–60 min, and produces long-lasting and far-reaching ocean waves and seismic signals, including ‘‘glacial earthquakes’’. Calvi...