© 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century. Information on outlet glacier dynamics, prior to this, are limited due to both a lack of observations and a paucity of mapped or mappable deglacial evidence which restricts our understanding of centennial to millennial timescale dynamics of the GrIS. Here ...
Recent rapid changes in the marine-terminating sectors of the Greenland Ice Sheet (GrIS) have prompt...
The Greenland Ice Sheet (GrIS) is a key component of the global climate system. However, our current...
Reports studies in 1959 and 1961 of glacial features in five valleys of this area (approx. 72 N, 24 ...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The centennial response of land-terminating glaciers in Greenland to climate change is largely unkno...
The Greenland Ice Sheet (GrIS) is losing mass in response to recent climatic and oceanic warming. Si...
In this study, we present new information on the glacial history of the Greenland Ice Sheet (GrIS) a...
The Greenland Ice Sheet (GrIS) is losing mass in response to recent climatic and oceanic warming. Si...
Significant uncertainty surrounds the influence of atmospheric and oceanic forcing on the fluctuatio...
Geophysical ice-sheet models are used to predict future ice-sheet dimensions and, in turn, these pro...
International audienceThe Greenland Ice Sheet (GrIS) plays a key role in the global climate system. ...
Over the last few decades atmospheric warming across the Arctic has been far more rapid than elsewhe...
This paper presents a new, detailed geomorphological and sedimentological appraisal of the southern ...
Recent rapid changes in the marine-terminating sectors of the Greenland Ice Sheet (GrIS) have prompt...
The Greenland Ice Sheet (GrIS) is a key component of the global climate system. However, our current...
Reports studies in 1959 and 1961 of glacial features in five valleys of this area (approx. 72 N, 24 ...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century...
The centennial response of land-terminating glaciers in Greenland to climate change is largely unkno...
The Greenland Ice Sheet (GrIS) is losing mass in response to recent climatic and oceanic warming. Si...
In this study, we present new information on the glacial history of the Greenland Ice Sheet (GrIS) a...
The Greenland Ice Sheet (GrIS) is losing mass in response to recent climatic and oceanic warming. Si...
Significant uncertainty surrounds the influence of atmospheric and oceanic forcing on the fluctuatio...
Geophysical ice-sheet models are used to predict future ice-sheet dimensions and, in turn, these pro...
International audienceThe Greenland Ice Sheet (GrIS) plays a key role in the global climate system. ...
Over the last few decades atmospheric warming across the Arctic has been far more rapid than elsewhe...
This paper presents a new, detailed geomorphological and sedimentological appraisal of the southern ...
Recent rapid changes in the marine-terminating sectors of the Greenland Ice Sheet (GrIS) have prompt...
The Greenland Ice Sheet (GrIS) is a key component of the global climate system. However, our current...
Reports studies in 1959 and 1961 of glacial features in five valleys of this area (approx. 72 N, 24 ...