Articles | Volume 13, issue 9
https://doi.org/10.5194/tc-13-2489-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-13-2489-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
26 Sep 2019
Research article | Highlight paper |
| 26 Sep 2019
| 26 Sep 2019
Estimating Greenland tidewater glacier retreat driven by submarine melting
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA
Fiamma Straneo
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA
Denis Felikson
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Christopher M. Little
Atmospheric and Environmental Research, Inc., Lexington, MA, USA
Heiko Goelzer
Utrecht University, Institute for Marine and Atmospheric Research, Utrecht, the Netherlands
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
Xavier Fettweis
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
James Holte
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA
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- Future Evolution of Greenland's Marine‐Terminating Outlet Glaciers G. Catania et al. 10.1029/2018JF004873
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- Return to rapid ice loss in Greenland and record loss in 2019 detected by the GRACE-FO satellites I. Sasgen et al. 10.1038/s43247-020-0010-1
- Advances in monitoring glaciological processes in Kalallit Nunaat (Greenland) over the past decades D. Fahrner et al. 10.1371/journal.pclm.0000379
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1 citations as recorded by crossref.
Latest update: 14 Dec 2024
Short summary
The ocean's influence on the retreat of Greenland's tidewater glaciers is a key factor determining future sea level. By considering observations of ~200 glaciers from 1960, we find a significant relationship between retreat and melting in the ocean. Projected forwards, this relationship estimates the future evolution of Greenland's tidewater glaciers and provides a practical and empirically validated way of representing ice–ocean interaction in large-scale models used to estimate sea level rise.
The ocean's influence on the retreat of Greenland's tidewater glaciers is a key factor...
Special issue