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...

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Published in:Geophysical Research Letters
Main Authors: David E. Gwyther, Christine F. Dow, Stefan Jendersie, Noel Gourmelen, Benjamin K. Galton‐Fenzi
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL103765
https://doaj.org/article/423cd08b56494dd8a72e6077d43cfb31
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spelling 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
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