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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Main Authors: Gagliardini, Olivier, Werder, Mauro
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2018
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000302286
http://hdl.handle.net/20.500.11850/302286
id ftdatacite:10.3929/ethz-b-000302286
record_format openpolar
spelling 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)
institution 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
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