This is the final version of the article. Available from AGU via the DOI in this record.Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the penetration of warm Atlantic water (AW) that rapidly melts and undercuts Greenland's marine-terminating glaciers. Here we present a new compilation of Greenland bed topography that assimilates seafloor bathymetry and ice thickness data through a mass conservation approach. A new 150 m horizontal resolution bed topography/bathymetric map of Greenland is constructed with seamless transitions at the ice/ocean interface, yielding major improvements over previous data sets, particularly in t...
Understanding the advance and retreat history of the northwest Greenland Ice Sheet (nwGIS) and its i...
The ocean plays an important role in modulating the mass balance of the polar ice sheets by interact...
This is the published version. Copyright 2013 European Geosciences UnionWe present a new bed elevati...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Greenland’s bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Melting of the Greenland Ice Sheet has the potential to raise sea level by 7.36 m and is already con...
Southeast Greenland has been a major participant in the ice sheet mass loss over the last several de...
Marine-terminating glaciers play a critical role in controlling Greenland's ice sheet mass balance. ...
Marine-terminating glaciers play a critical role in controlling Greenland's ice sheet mass balance. ...
A new digital bathymetric model (DBM) for the Northeast Greenland (NEG) continental shelf (74°N–81°N...
Storstrømmen and L. Bistrup Bræ are 20- and 10-km wide, surge type glaciers in North Greenland in qu...
Bed topography is a critical boundary for the numerical modelling of ice sheets and ice-ocean intera...
Understanding the advance and retreat history of the northwest Greenland Ice Sheet (nwGIS) and its i...
The ocean plays an important role in modulating the mass balance of the polar ice sheets by interact...
This is the published version. Copyright 2013 European Geosciences UnionWe present a new bed elevati...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Greenland’s bed topography is a primary control on ice flow, grounding line migration, calving dynam...
Melting of the Greenland Ice Sheet has the potential to raise sea level by 7.36 m and is already con...
Southeast Greenland has been a major participant in the ice sheet mass loss over the last several de...
Marine-terminating glaciers play a critical role in controlling Greenland's ice sheet mass balance. ...
Marine-terminating glaciers play a critical role in controlling Greenland's ice sheet mass balance. ...
A new digital bathymetric model (DBM) for the Northeast Greenland (NEG) continental shelf (74°N–81°N...
Storstrømmen and L. Bistrup Bræ are 20- and 10-km wide, surge type glaciers in North Greenland in qu...
Bed topography is a critical boundary for the numerical modelling of ice sheets and ice-ocean intera...
Understanding the advance and retreat history of the northwest Greenland Ice Sheet (nwGIS) and its i...
The ocean plays an important role in modulating the mass balance of the polar ice sheets by interact...
This is the published version. Copyright 2013 European Geosciences UnionWe present a new bed elevati...