Geometric controls of tidewater glacier dynamics

Retreat of marine outlet glaciers often initiates depletion of inland ice through dynamic adjustments of the upstream glacier. The local topography of a fjord may promote or inhibit such retreat, and therefore fjord geometry constitutes a critical control on ice sheet mass balance. To quantify the p...

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Published in:The Cryosphere
Main Authors: Frank, Thomas, Åkesson, Henning, Fleurian, Basile de, Morlighem, M., Nisancioglu, Kerim Hestnes
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://hdl.handle.net/11250/2984317
https://doi.org/10.5194/tc-16-581-2022
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spelling ftunivbergen:oai:bora.uib.no:11250/2984317 2023-05-15T16:40:37+02:00 Geometric controls of tidewater glacier dynamics Frank, Thomas Åkesson, Henning Fleurian, Basile de Morlighem, M. Nisancioglu, Kerim Hestnes 2022 application/pdf https://hdl.handle.net/11250/2984317 https://doi.org/10.5194/tc-16-581-2022 eng eng Copernicus Publications Notur/NorStore: nn4659k Norges forskningsråd: 302458 Norges forskningsråd: 287206 Notur/NorStore: ns4659k Notur/NorStore: nn9635k Notur/NorStore: ns9635k urn:issn:1994-0416 https://hdl.handle.net/11250/2984317 https://doi.org/10.5194/tc-16-581-2022 cristin:2003311 The Cryosphere. 2022, 16 (2), 581-601. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright Author(s) 2022 The Cryosphere 581-601 16 2 Journal article Peer reviewed 2022 ftunivbergen https://doi.org/10.5194/tc-16-581-2022 2023-03-14T17:41:08Z Retreat of marine outlet glaciers often initiates depletion of inland ice through dynamic adjustments of the upstream glacier. The local topography of a fjord may promote or inhibit such retreat, and therefore fjord geometry constitutes a critical control on ice sheet mass balance. To quantify the processes of ice–topography interactions and enhance the understanding of the dynamics involved, we analyze a multitude of topographic fjord settings and scenarios using the Ice-sheet and Sea-level System Model (ISSM). We systematically study glacier retreat through a variety of artificial fjord geometries and quantify the modeled dynamics directly in relation to topographic features. We find that retreat in an upstream-widening or upstream-deepening fjord does not necessarily promote retreat, as suggested by previous studies. Conversely, it may stabilize a glacier because converging ice flow towards a constriction enhances lateral and basal shear stress gradients. An upstream-narrowing or upstream-shoaling fjord, in turn, may promote retreat since fjord walls or bed provide little stability to the glacier where ice flow diverges. Furthermore, we identify distinct quantitative relationships directly linking grounding line discharge and retreat rate to fjord topography and transfer these results to a long-term study of the retreat of Jakobshavn Isbræ. These findings offer new perspectives on ice–topography interactions and give guidance to an ad hoc assessment of future topographically induced ice loss based on knowledge of the upstream fjord geometry. publishedVersion Article in Journal/Newspaper Ice Sheet Jakobshavn Jakobshavn isbræ The Cryosphere Tidewater University of Bergen: Bergen Open Research Archive (BORA-UiB) Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) The Cryosphere 16 2 581 601
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description Retreat of marine outlet glaciers often initiates depletion of inland ice through dynamic adjustments of the upstream glacier. The local topography of a fjord may promote or inhibit such retreat, and therefore fjord geometry constitutes a critical control on ice sheet mass balance. To quantify the processes of ice–topography interactions and enhance the understanding of the dynamics involved, we analyze a multitude of topographic fjord settings and scenarios using the Ice-sheet and Sea-level System Model (ISSM). We systematically study glacier retreat through a variety of artificial fjord geometries and quantify the modeled dynamics directly in relation to topographic features. We find that retreat in an upstream-widening or upstream-deepening fjord does not necessarily promote retreat, as suggested by previous studies. Conversely, it may stabilize a glacier because converging ice flow towards a constriction enhances lateral and basal shear stress gradients. An upstream-narrowing or upstream-shoaling fjord, in turn, may promote retreat since fjord walls or bed provide little stability to the glacier where ice flow diverges. Furthermore, we identify distinct quantitative relationships directly linking grounding line discharge and retreat rate to fjord topography and transfer these results to a long-term study of the retreat of Jakobshavn Isbræ. These findings offer new perspectives on ice–topography interactions and give guidance to an ad hoc assessment of future topographically induced ice loss based on knowledge of the upstream fjord geometry. publishedVersion
format Article in Journal/Newspaper
author Frank, Thomas
Åkesson, Henning
Fleurian, Basile de
Morlighem, M.
Nisancioglu, Kerim Hestnes
spellingShingle Frank, Thomas
Åkesson, Henning
Fleurian, Basile de
Morlighem, M.
Nisancioglu, Kerim Hestnes
Geometric controls of tidewater glacier dynamics
author_facet Frank, Thomas
Åkesson, Henning
Fleurian, Basile de
Morlighem, M.
Nisancioglu, Kerim Hestnes
author_sort Frank, Thomas
title Geometric controls of tidewater glacier dynamics
title_short Geometric controls of tidewater glacier dynamics
title_full Geometric controls of tidewater glacier dynamics
title_fullStr Geometric controls of tidewater glacier dynamics
title_full_unstemmed Geometric controls of tidewater glacier dynamics
title_sort geometric controls of tidewater glacier dynamics
publisher Copernicus Publications
publishDate 2022
url https://hdl.handle.net/11250/2984317
https://doi.org/10.5194/tc-16-581-2022
long_lat ENVELOPE(-49.917,-49.917,69.167,69.167)
geographic Jakobshavn Isbræ
geographic_facet Jakobshavn Isbræ
genre Ice Sheet
Jakobshavn
Jakobshavn isbræ
The Cryosphere
Tidewater
genre_facet Ice Sheet
Jakobshavn
Jakobshavn isbræ
The Cryosphere
Tidewater
op_source The Cryosphere
581-601
16
2
op_relation Notur/NorStore: nn4659k
Norges forskningsråd: 302458
Norges forskningsråd: 287206
Notur/NorStore: ns4659k
Notur/NorStore: nn9635k
Notur/NorStore: ns9635k
urn:issn:1994-0416
https://hdl.handle.net/11250/2984317
https://doi.org/10.5194/tc-16-581-2022
cristin:2003311
The Cryosphere. 2022, 16 (2), 581-601.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
Copyright Author(s) 2022
op_doi https://doi.org/10.5194/tc-16-581-2022
container_title The Cryosphere
container_volume 16
container_issue 2
container_start_page 581
op_container_end_page 601
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