Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ...
Over recent decades, Greenland ice sheet surface melt has shown an increase both in intensity and spatial extent. Part of this water probably reaches the bed and can enhance glacier speed, advecting a larger volume of ice into the ablation area. In the context of a warming climate, this mechanism co...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000302286 http://hdl.handle.net/20.500.11850/302286 |
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ftdatacite:10.3929/ethz-b-000302286 2024-04-28T08:19:49+00:00 Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... Gagliardini, Olivier Werder, Mauro 2018 application/pdf https://dx.doi.org/10.3929/ethz-b-000302286 http://hdl.handle.net/20.500.11850/302286 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Crevasses glacier modelling subglacial processes article-journal Text ScholarlyArticle Journal Article 2018 ftdatacite https://doi.org/10.3929/ethz-b-000302286 2024-04-02T12:33:25Z Over recent decades, Greenland ice sheet surface melt has shown an increase both in intensity and spatial extent. Part of this water probably reaches the bed and can enhance glacier speed, advecting a larger volume of ice into the ablation area. In the context of a warming climate, this mechanism could contribute to the future rate of thinning and retreat of land-terminating glaciers of Greenland. These changes in ice flow conditions will in turn influence surface crevassing and thus the ability of water to reach the bed at higher elevations. Here, using a coupled basal hydrology and prognostic ice flow model, the evolution of a Greenland-type glacier subject to increasing surface melt is studied over a few decades. For different scenarios of surface melt increase over the next decades, the evolution of crevassed areas and the ability of water to reach the bed is inferred. Our results indicate that the currently observed crevasse distribution is likely to extend further upstream which will allow water to ... : Journal of Glaciology, 64 (247) ... Article in Journal/Newspaper glacier Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Crevasses glacier modelling subglacial processes |
spellingShingle |
Crevasses glacier modelling subglacial processes Gagliardini, Olivier Werder, Mauro Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
topic_facet |
Crevasses glacier modelling subglacial processes |
description |
Over recent decades, Greenland ice sheet surface melt has shown an increase both in intensity and spatial extent. Part of this water probably reaches the bed and can enhance glacier speed, advecting a larger volume of ice into the ablation area. In the context of a warming climate, this mechanism could contribute to the future rate of thinning and retreat of land-terminating glaciers of Greenland. These changes in ice flow conditions will in turn influence surface crevassing and thus the ability of water to reach the bed at higher elevations. Here, using a coupled basal hydrology and prognostic ice flow model, the evolution of a Greenland-type glacier subject to increasing surface melt is studied over a few decades. For different scenarios of surface melt increase over the next decades, the evolution of crevassed areas and the ability of water to reach the bed is inferred. Our results indicate that the currently observed crevasse distribution is likely to extend further upstream which will allow water to ... : Journal of Glaciology, 64 (247) ... |
format |
Article in Journal/Newspaper |
author |
Gagliardini, Olivier Werder, Mauro |
author_facet |
Gagliardini, Olivier Werder, Mauro |
author_sort |
Gagliardini, Olivier |
title |
Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
title_short |
Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
title_full |
Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
title_fullStr |
Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
title_full_unstemmed |
Influence of increasing surface melt over decadal timescales on land-terminating Greenland-type outlet glaciers ... |
title_sort |
influence of increasing surface melt over decadal timescales on land-terminating greenland-type outlet glaciers ... |
publisher |
ETH Zurich |
publishDate |
2018 |
url |
https://dx.doi.org/10.3929/ethz-b-000302286 http://hdl.handle.net/20.500.11850/302286 |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000302286 |
_version_ |
1797583104288751616 |