Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow
Abstract Future projections of global mean sea level change are uncertain, partly because of our limited understanding of the dynamics of Greenland’s outlet glaciers. Here we study Nioghalvfjerdsbræ, an outlet glacier of the Northeast Greenland Ice Stream that holds 1.1 m sea-level equivalent of ice...
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2021
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Online Access: | http://dx.doi.org/10.1038/s43247-021-00296-3 https://www.nature.com/articles/s43247-021-00296-3.pdf https://www.nature.com/articles/s43247-021-00296-3 |
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crspringernat:10.1038/s43247-021-00296-3 2023-05-15T16:21:02+02:00 Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow Christmann, Julia Helm, Veit Khan, Shfaqat Abbas Kleiner, Thomas Müller, Ralf Morlighem, Mathieu Neckel, Niklas Rückamp, Martin Steinhage, Daniel Zeising, Ole Humbert, Angelika Bundesministerium für Bildung und Forschung European Union’s Horizon 2020 Research and Innovation Programme 2021 http://dx.doi.org/10.1038/s43247-021-00296-3 https://www.nature.com/articles/s43247-021-00296-3.pdf https://www.nature.com/articles/s43247-021-00296-3 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Communications Earth & Environment volume 2, issue 1 ISSN 2662-4435 General Earth and Planetary Sciences General Environmental Science journal-article 2021 crspringernat https://doi.org/10.1038/s43247-021-00296-3 2022-01-04T07:40:54Z Abstract Future projections of global mean sea level change are uncertain, partly because of our limited understanding of the dynamics of Greenland’s outlet glaciers. Here we study Nioghalvfjerdsbræ, an outlet glacier of the Northeast Greenland Ice Stream that holds 1.1 m sea-level equivalent of ice. We use GPS observations and numerical modelling to investigate the role of tides as well as the elastic contribution to glacier flow. We find that ocean tides alter the basal lubrication of the glacier up to 10 km inland of the grounding line, and that their influence is best described by a viscoelastic rather than a viscous model. Further inland, sliding is the dominant mechanism of fast glacier motion, and the ice flow induces persistent elastic strain. We conclude that elastic deformation plays a role in glacier flow, particularly in areas of steep topographic changes and fast ice velocities. Article in Journal/Newspaper glacier Greenland Springer Nature (via Crossref) Greenland Communications Earth & Environment 2 1 |
institution |
Open Polar |
collection |
Springer Nature (via Crossref) |
op_collection_id |
crspringernat |
language |
English |
topic |
General Earth and Planetary Sciences General Environmental Science |
spellingShingle |
General Earth and Planetary Sciences General Environmental Science Christmann, Julia Helm, Veit Khan, Shfaqat Abbas Kleiner, Thomas Müller, Ralf Morlighem, Mathieu Neckel, Niklas Rückamp, Martin Steinhage, Daniel Zeising, Ole Humbert, Angelika Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
topic_facet |
General Earth and Planetary Sciences General Environmental Science |
description |
Abstract Future projections of global mean sea level change are uncertain, partly because of our limited understanding of the dynamics of Greenland’s outlet glaciers. Here we study Nioghalvfjerdsbræ, an outlet glacier of the Northeast Greenland Ice Stream that holds 1.1 m sea-level equivalent of ice. We use GPS observations and numerical modelling to investigate the role of tides as well as the elastic contribution to glacier flow. We find that ocean tides alter the basal lubrication of the glacier up to 10 km inland of the grounding line, and that their influence is best described by a viscoelastic rather than a viscous model. Further inland, sliding is the dominant mechanism of fast glacier motion, and the ice flow induces persistent elastic strain. We conclude that elastic deformation plays a role in glacier flow, particularly in areas of steep topographic changes and fast ice velocities. |
author2 |
Bundesministerium für Bildung und Forschung European Union’s Horizon 2020 Research and Innovation Programme |
format |
Article in Journal/Newspaper |
author |
Christmann, Julia Helm, Veit Khan, Shfaqat Abbas Kleiner, Thomas Müller, Ralf Morlighem, Mathieu Neckel, Niklas Rückamp, Martin Steinhage, Daniel Zeising, Ole Humbert, Angelika |
author_facet |
Christmann, Julia Helm, Veit Khan, Shfaqat Abbas Kleiner, Thomas Müller, Ralf Morlighem, Mathieu Neckel, Niklas Rückamp, Martin Steinhage, Daniel Zeising, Ole Humbert, Angelika |
author_sort |
Christmann, Julia |
title |
Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
title_short |
Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
title_full |
Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
title_fullStr |
Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
title_full_unstemmed |
Elastic deformation plays a non-negligible role in Greenland’s outlet glacier flow |
title_sort |
elastic deformation plays a non-negligible role in greenland’s outlet glacier flow |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1038/s43247-021-00296-3 https://www.nature.com/articles/s43247-021-00296-3.pdf https://www.nature.com/articles/s43247-021-00296-3 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland |
genre_facet |
glacier Greenland |
op_source |
Communications Earth & Environment volume 2, issue 1 ISSN 2662-4435 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s43247-021-00296-3 |
container_title |
Communications Earth & Environment |
container_volume |
2 |
container_issue |
1 |
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1766009043965444096 |