Articles | Volume 11, issue 2
https://doi.org/10.5194/tc-11-1015-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/tc-11-1015-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Reconstructions of the 1900–2015 Greenland ice sheet surface mass balance using the regional climate MAR model
Xavier Fettweis
CORRESPONDING AUTHOR
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Jason E. Box
Department of Glaciology and Climate, Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark
Cécile Agosta
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Charles Amory
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Christoph Kittel
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Charlotte Lang
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Dirk van As
Department of Glaciology and Climate, Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark
Horst Machguth
Department of Geography, University of Zurich, Zurich, Switzerland
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Hubert Gallée
Laboratoire de Glaciologie et Géophysique de l'Environnement (LGGE), Grenoble, France
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- Predicting the loss of organic archaeological deposits at a regional scale in Greenland J. Hollesen et al. 10.1038/s41598-019-45200-4
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4 citations as recorded by crossref.
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Discussed (preprint)
Latest update: 17 Nov 2024
Short summary
This paper shows that the surface melt increase over the Greenland ice sheet since the end of the 1990s has been unprecedented, with respect to the last 120 years, using a regional climate model. These simulations also suggest an increase of the snowfall accumulation through the last century before a surface mass decrease in the 2000s. Such a mass gain could have impacted the ice sheet's dynamic stability and could explain the recent observed increase of the glaciers' velocity.
This paper shows that the surface melt increase over the Greenland ice sheet since the end of...
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