Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf
Abstract Subglacial freshwater discharge from beneath Antarctic glaciers likely has a strong impact on ice shelf basal melting. However, the difficulty in directly observing subglacial flow highlights the importance of modeling these processes. We use an ocean model of the Totten Ice Shelf cavity in...
Published in: | Geophysical Research Letters |
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Online Access: | https://doi.org/10.1029/2023GL103765 https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31 |
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ftdoajarticles:oai:doaj.org/article:423cd08b56494dd8a72e6077d43cfb31 2024-09-15T17:44:39+00:00 Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf David E. Gwyther Christine F. Dow Stefan Jendersie Noel Gourmelen Benjamin K. Galton‐Fenzi 2023-06-01T00:00:00Z https://doi.org/10.1029/2023GL103765 https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31 EN eng Wiley https://doi.org/10.1029/2023GL103765 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103765 https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31 Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023) basal melting subglacial discharge Totten ice shelf Antarctica ice shelves sea level rise Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL103765 2024-08-05T17:49:23Z Abstract Subglacial freshwater discharge from beneath Antarctic glaciers likely has a strong impact on ice shelf basal melting. However, the difficulty in directly observing subglacial flow highlights the importance of modeling these processes. We use an ocean model of the Totten Ice Shelf cavity into which we inject subglacial discharge derived from a hydrology model applied to Aurora Subglacial Basin. Our results show (a) discharge increases melting in the vicinity of the outflow region, which correlates with features observed in surface elevation maps and satellite‐derived melt maps, with implications for ice shelf stability; (b) the change in melting is driven by the formation of a buoyant plume rather than the addition of heat; and (c) the buoyant plume originating from subglacial discharge‐driven melting is far‐reaching. Basal melting induced by subglacial hydrology is thus important for ice shelf stability, but is absent from almost all ice‐ocean models. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Shelf Ice Shelves Totten Ice Shelf Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 12 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
basal melting subglacial discharge Totten ice shelf Antarctica ice shelves sea level rise Geophysics. Cosmic physics QC801-809 |
spellingShingle |
basal melting subglacial discharge Totten ice shelf Antarctica ice shelves sea level rise Geophysics. Cosmic physics QC801-809 David E. Gwyther Christine F. Dow Stefan Jendersie Noel Gourmelen Benjamin K. Galton‐Fenzi Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
topic_facet |
basal melting subglacial discharge Totten ice shelf Antarctica ice shelves sea level rise Geophysics. Cosmic physics QC801-809 |
description |
Abstract Subglacial freshwater discharge from beneath Antarctic glaciers likely has a strong impact on ice shelf basal melting. However, the difficulty in directly observing subglacial flow highlights the importance of modeling these processes. We use an ocean model of the Totten Ice Shelf cavity into which we inject subglacial discharge derived from a hydrology model applied to Aurora Subglacial Basin. Our results show (a) discharge increases melting in the vicinity of the outflow region, which correlates with features observed in surface elevation maps and satellite‐derived melt maps, with implications for ice shelf stability; (b) the change in melting is driven by the formation of a buoyant plume rather than the addition of heat; and (c) the buoyant plume originating from subglacial discharge‐driven melting is far‐reaching. Basal melting induced by subglacial hydrology is thus important for ice shelf stability, but is absent from almost all ice‐ocean models. |
format |
Article in Journal/Newspaper |
author |
David E. Gwyther Christine F. Dow Stefan Jendersie Noel Gourmelen Benjamin K. Galton‐Fenzi |
author_facet |
David E. Gwyther Christine F. Dow Stefan Jendersie Noel Gourmelen Benjamin K. Galton‐Fenzi |
author_sort |
David E. Gwyther |
title |
Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
title_short |
Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
title_full |
Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
title_fullStr |
Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
title_full_unstemmed |
Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf |
title_sort |
subglacial freshwater drainage increases simulated basal melt of the totten ice shelf |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2023GL103765 https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31 |
genre |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves Totten Ice Shelf |
genre_facet |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves Totten Ice Shelf |
op_source |
Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2023GL103765 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL103765 https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31 |
op_doi |
https://doi.org/10.1029/2023GL103765 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
12 |
_version_ |
1810492307472908288 |