Storstrømmen and L. Bistrup Bræ are 20- and 10-km wide, surge type glaciers in North Greenland in quiescent phase that terminate in the southernmost floating ice tongue in East Greenland. Novel multi-beam echo sounding data collected in August 2020 indicate a seabed at 350–400 m depth along a relatively uniform ice shelf front, 100 m deeper than expected, but surrounded by shallower terrain (<100 m) over a 30-km wide region that blocks the access of warm, salty, subsurface Atlantic Intermediate Water (AIW) at +1.6°C. Conductivity temperature depth data reveal waters in front of the glaciers at −1.8°C not connected to AIW in the outer fjord, Dove Bugt. The recent grounding line retreat of the glaciers is attributed to glacier thinning at its...
This is the final version of the article. Available from AGU via the DOI in this record.Greenland's ...
Mass loss from the Greenland ice sheet has increased over the past two decades, currently accounting...
Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduc...
Storstrømmen and L. Bistrup Bræ are 20- and 10-km wide, surge type glaciers in North Greenland in qu...
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. ...
Author Posting. © Geological Survey of Denmark and Greenland, 2014. This article is posted here by ...
The Northeast Greenland Ice Stream has recently seen significant change to its floating margins and ...
Southeast Greenland has been a major participant in the ice sheet mass loss over the last several de...
Warming of subsurface water of Atlantic origin has been suggested to be a major driver of the ongoin...
Hydrographic data collected during five summer surveys between 2002 and 2015 reveal that the subsurf...
The thinning, acceleration, and retreat of Greenland glaciers since the mid-1990s has been attribute...
It is well known that warming of deep Atlantic Water in recent decades resulted in extensive retreat...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
The research under project CALISMO (Calving Laws for Ice Sheet Models) was funded by the Natural Env...
This is the final version of the article. Available from AGU via the DOI in this record.Greenland's ...
Mass loss from the Greenland ice sheet has increased over the past two decades, currently accounting...
Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduc...
Storstrømmen and L. Bistrup Bræ are 20- and 10-km wide, surge type glaciers in North Greenland in qu...
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. ...
Author Posting. © Geological Survey of Denmark and Greenland, 2014. This article is posted here by ...
The Northeast Greenland Ice Stream has recently seen significant change to its floating margins and ...
Southeast Greenland has been a major participant in the ice sheet mass loss over the last several de...
Warming of subsurface water of Atlantic origin has been suggested to be a major driver of the ongoin...
Hydrographic data collected during five summer surveys between 2002 and 2015 reveal that the subsurf...
The thinning, acceleration, and retreat of Greenland glaciers since the mid-1990s has been attribute...
It is well known that warming of deep Atlantic Water in recent decades resulted in extensive retreat...
© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attributi...
The research under project CALISMO (Calving Laws for Ice Sheet Models) was funded by the Natural Env...
This is the final version of the article. Available from AGU via the DOI in this record.Greenland's ...
Mass loss from the Greenland ice sheet has increased over the past two decades, currently accounting...
Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduc...