Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell

Understanding the causes of recent catastrophic ice shelf disintegrations is a crucial step towards improving coupled models of the Antarctic Ice Sheet and predicting its future state and contribution to sea-level rise. An overlooked climate-related causal factor is regional sea ice loss. Here we sh...

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Published in:Nature
Main Authors: Massom, RA, Scambos, TA, Bennetts, LG, Reid, P, Squire, VA, Stammerjohn, SE
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2018
Subjects:
Online Access:https://eprints.utas.edu.au/39491/
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spelling ftunivtasmania:oai:eprints.utas.edu.au:39491 2023-05-15T13:42:39+02:00 Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell Massom, RA Scambos, TA Bennetts, LG Reid, P Squire, VA Stammerjohn, SE 2018 https://eprints.utas.edu.au/39491/ unknown Nature Publishing Group Massom, RA orcid:0000-0003-1533-5084 , Scambos, TA, Bennetts, LG, Reid, P, Squire, VA and Stammerjohn, SE 2018 , 'Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell' , Nature, vol. 558, no. 7710 , pp. 383-389 , doi:10.1038/s41586-018-0212-1 <http://dx.doi.org/10.1038/s41586-018-0212-1>. Antarctic ice shelf disintegration sea ice change ocean swell Article PeerReviewed 2018 ftunivtasmania https://doi.org/10.1038/s41586-018-0212-1 2022-01-17T23:17:43Z Understanding the causes of recent catastrophic ice shelf disintegrations is a crucial step towards improving coupled models of the Antarctic Ice Sheet and predicting its future state and contribution to sea-level rise. An overlooked climate-related causal factor is regional sea ice loss. Here we show that for the disintegration events observed (the collapse of the Larsen A and B and Wilkins ice shelves), the increased seasonal absence of a protective sea ice buffer enabled increased flexure of vulnerable outer ice shelf margins by ocean swells that probably weakened them to the point of calving. This outer-margin calving triggered wider-scale disintegration of ice shelves compromised by multiple factors in preceding years, with key prerequisites being extensive flooding and outer-margin fracturing. Wave-induced flexure is particularly effective in outermost ice shelf regions thinned by bottom crevassing. Our analysis of satellite and ocean-wave data and modelling of combined ice shelf, sea ice and wave properties highlights the need for ice sheet models to account for sea ice and ocean waves. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Sea ice University of Tasmania: UTas ePrints Antarctic The Antarctic Wilkins ENVELOPE(59.326,59.326,-67.248,-67.248) Nature 558 7710 383 389
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language unknown
topic Antarctic
ice shelf
disintegration
sea ice
change
ocean swell
spellingShingle Antarctic
ice shelf
disintegration
sea ice
change
ocean swell
Massom, RA
Scambos, TA
Bennetts, LG
Reid, P
Squire, VA
Stammerjohn, SE
Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
topic_facet Antarctic
ice shelf
disintegration
sea ice
change
ocean swell
description Understanding the causes of recent catastrophic ice shelf disintegrations is a crucial step towards improving coupled models of the Antarctic Ice Sheet and predicting its future state and contribution to sea-level rise. An overlooked climate-related causal factor is regional sea ice loss. Here we show that for the disintegration events observed (the collapse of the Larsen A and B and Wilkins ice shelves), the increased seasonal absence of a protective sea ice buffer enabled increased flexure of vulnerable outer ice shelf margins by ocean swells that probably weakened them to the point of calving. This outer-margin calving triggered wider-scale disintegration of ice shelves compromised by multiple factors in preceding years, with key prerequisites being extensive flooding and outer-margin fracturing. Wave-induced flexure is particularly effective in outermost ice shelf regions thinned by bottom crevassing. Our analysis of satellite and ocean-wave data and modelling of combined ice shelf, sea ice and wave properties highlights the need for ice sheet models to account for sea ice and ocean waves.
format Article in Journal/Newspaper
author Massom, RA
Scambos, TA
Bennetts, LG
Reid, P
Squire, VA
Stammerjohn, SE
author_facet Massom, RA
Scambos, TA
Bennetts, LG
Reid, P
Squire, VA
Stammerjohn, SE
author_sort Massom, RA
title Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
title_short Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
title_full Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
title_fullStr Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
title_full_unstemmed Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
title_sort antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
publisher Nature Publishing Group
publishDate 2018
url https://eprints.utas.edu.au/39491/
long_lat ENVELOPE(59.326,59.326,-67.248,-67.248)
geographic Antarctic
The Antarctic
Wilkins
geographic_facet Antarctic
The Antarctic
Wilkins
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Sea ice
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
Sea ice
op_relation Massom, RA orcid:0000-0003-1533-5084 , Scambos, TA, Bennetts, LG, Reid, P, Squire, VA and Stammerjohn, SE 2018 , 'Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell' , Nature, vol. 558, no. 7710 , pp. 383-389 , doi:10.1038/s41586-018-0212-1 <http://dx.doi.org/10.1038/s41586-018-0212-1>.
op_doi https://doi.org/10.1038/s41586-018-0212-1
container_title Nature
container_volume 558
container_issue 7710
container_start_page 383
op_container_end_page 389
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