Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations

Major ice loss has recently been observed along coastal outlet glaciers of the West Antarctic ice sheet, mainly due to increased melting below the ice shelves. However, the behavior of this marine ice sheet is poorly understood, leading to significant shortcomings in ice-sheet models attempting to p...

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Published in:Journal of Glaciology
Main Authors: Docquier, David, Pollard, David, Pattyn, Frank
Other Authors: Université Libre de Bruxelles - Laboratoire de Glaciologie, Pennsylvania State University - Earth and Environmental Systems Institute, UCL - SST/ELI/ELIC - Earth & Climate
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2014
Subjects:
Online Access:http://hdl.handle.net/2078/167215
https://doi.org/10.3189/2014JoG13J117
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spelling ftunivlouvain:oai:dial.uclouvain.be:boreal:167215 2024-05-12T07:52:50+00:00 Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations Docquier, David Pollard, David Pattyn, Frank Université Libre de Bruxelles - Laboratoire de Glaciologie Pennsylvania State University - Earth and Environmental Systems Institute UCL - SST/ELI/ELIC - Earth & Climate 2014 http://hdl.handle.net/2078/167215 https://doi.org/10.3189/2014JoG13J117 eng eng International Glaciological Society boreal:167215 http://hdl.handle.net/2078/167215 doi:10.3189/2014JoG13J117 urn:ISSN:0022-1430 urn:EISSN:1727-5652 info:eu-repo/semantics/openAccess Journal of Glaciology, Vol. 60, no.220, p. 305-313 (2014) glacier flow ice dynamics ice-sheet modeling info:eu-repo/semantics/article 2014 ftunivlouvain https://doi.org/10.3189/2014JoG13J117 2024-04-17T17:07:53Z Major ice loss has recently been observed along coastal outlet glaciers of the West Antarctic ice sheet, mainly due to increased melting below the ice shelves. However, the behavior of this marine ice sheet is poorly understood, leading to significant shortcomings in ice-sheet models attempting to predict future sea-level rise. The stability of a marine ice sheet is controlled by the dynamics at the grounding line, the boundary between the grounded ice stream and the floating ice shelf. One of the largest contributors to current sea-level rise is the fast-flowing Thwaites Glacier, which flows into the Amundsen Sea. Here we use an ice-stream/ice-shelf model and perform a number of experiments along a central flowline to analyze the sensitivity of its grounding line on centennial timescales. In the absence of width and buttressing effects, we find that the grounding line retreats by ∼300 km in 200 years from the present day (rate of 1.5 km a–1). With variable glacier width implemented in the model, flow convergence slows the retreat of Thwaites grounding line at 0.3–1.2 km a–1. The parameterization of ice-shelf buttressing according to different observed scenarios further reduces the glacier retreat and can even lead to a slight advance in the most buttressed case. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Thwaites Glacier DIAL@UCLouvain (Université catholique de Louvain) Amundsen Sea Antarctic Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) West Antarctic Ice Sheet Journal of Glaciology 60 220 305 313
institution Open Polar
collection DIAL@UCLouvain (Université catholique de Louvain)
op_collection_id ftunivlouvain
language English
topic glacier flow
ice dynamics
ice-sheet modeling
spellingShingle glacier flow
ice dynamics
ice-sheet modeling
Docquier, David
Pollard, David
Pattyn, Frank
Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
topic_facet glacier flow
ice dynamics
ice-sheet modeling
description Major ice loss has recently been observed along coastal outlet glaciers of the West Antarctic ice sheet, mainly due to increased melting below the ice shelves. However, the behavior of this marine ice sheet is poorly understood, leading to significant shortcomings in ice-sheet models attempting to predict future sea-level rise. The stability of a marine ice sheet is controlled by the dynamics at the grounding line, the boundary between the grounded ice stream and the floating ice shelf. One of the largest contributors to current sea-level rise is the fast-flowing Thwaites Glacier, which flows into the Amundsen Sea. Here we use an ice-stream/ice-shelf model and perform a number of experiments along a central flowline to analyze the sensitivity of its grounding line on centennial timescales. In the absence of width and buttressing effects, we find that the grounding line retreats by ∼300 km in 200 years from the present day (rate of 1.5 km a–1). With variable glacier width implemented in the model, flow convergence slows the retreat of Thwaites grounding line at 0.3–1.2 km a–1. The parameterization of ice-shelf buttressing according to different observed scenarios further reduces the glacier retreat and can even lead to a slight advance in the most buttressed case.
author2 Université Libre de Bruxelles - Laboratoire de Glaciologie
Pennsylvania State University - Earth and Environmental Systems Institute
UCL - SST/ELI/ELIC - Earth & Climate
format Article in Journal/Newspaper
author Docquier, David
Pollard, David
Pattyn, Frank
author_facet Docquier, David
Pollard, David
Pattyn, Frank
author_sort Docquier, David
title Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
title_short Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
title_full Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
title_fullStr Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
title_full_unstemmed Thwaites Glacier grounding-line retreat: influence of width and buttressing parameterizations
title_sort thwaites glacier grounding-line retreat: influence of width and buttressing parameterizations
publisher International Glaciological Society
publishDate 2014
url http://hdl.handle.net/2078/167215
https://doi.org/10.3189/2014JoG13J117
long_lat ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Amundsen Sea
Antarctic
Thwaites Glacier
West Antarctic Ice Sheet
geographic_facet Amundsen Sea
Antarctic
Thwaites Glacier
West Antarctic Ice Sheet
genre Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
Thwaites Glacier
genre_facet Amundsen Sea
Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
Thwaites Glacier
op_source Journal of Glaciology, Vol. 60, no.220, p. 305-313 (2014)
op_relation boreal:167215
http://hdl.handle.net/2078/167215
doi:10.3189/2014JoG13J117
urn:ISSN:0022-1430
urn:EISSN:1727-5652
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.3189/2014JoG13J117
container_title Journal of Glaciology
container_volume 60
container_issue 220
container_start_page 305
op_container_end_page 313
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