Circulation and Ocean Driven Glacial Melting in a Greenland Fjord

Deglaciation of a marine-based ice sheet: Late Weichselian palaeo-ice dynamics and retreat in the southern Barents Sea reconstructed from onshore and offshore glacial geomorphology.

Here, we study the effect of subglacial water on past Eurasian ice-sheet dynamics by incorpor- ating a thin-film model of basal water flow into the ice-sheet model SICOPOLIS and use

The model accounts for the melting driven by modified WDW flowing into the ice shelf cavities, which is the main heat source in winter when the water column has temperatures close

The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry

The floating ice shelf of Peterman Glacier, one of four major outlet glaciers in Greenland, interacts directly with the ocean. Basal melting is confirmed by in-situ surveys to be

We have developed a physically based sea-ice albedo parameterization scheme for ECHAM5 GCM following the structure of the sea-ice albedo in a thermo- dynamic sea-ice model [Schramm

Although our approach lacks coupling between subglacial melt- water and ice dynamics, the abundance of predicted subglacial lakes connected to these modelled ice streams show

The numerical model is forced with a linear increase in surface mass balance, submarine melt rate, crevasse water depth and a reduction in sea ice buttressing to isolate the