Ice-shelf buttressing and the stability of marine ice sheets

Ice-shelf buttressing and the stability of marine-type ice sheets are investigated numerically. Buttressing effects are analysed for a situation where a stable grounding line is located on a bed sloping upwards in the direction of flow. Such grounding-line positions are known to be unconditionally u...

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Published in:The Cryosphere
Main Author: Gudmundsson, G. H.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-7-647-2013
https://tc.copernicus.org/articles/7/647/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:tc16627 2023-05-15T16:41:46+02:00 Ice-shelf buttressing and the stability of marine ice sheets Gudmundsson, G. H. 2018-09-27 application/pdf https://doi.org/10.5194/tc-7-647-2013 https://tc.copernicus.org/articles/7/647/2013/ eng eng doi:10.5194/tc-7-647-2013 https://tc.copernicus.org/articles/7/647/2013/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-7-647-2013 2020-07-20T16:25:31Z Ice-shelf buttressing and the stability of marine-type ice sheets are investigated numerically. Buttressing effects are analysed for a situation where a stable grounding line is located on a bed sloping upwards in the direction of flow. Such grounding-line positions are known to be unconditionally unstable in the absence of transverse flow variations. It is shown that ice-shelf buttressing can restore stability under these conditions. Ice flux at the grounding line is, in general, not a monotonically increasing function of ice thickness. This, possibly at first somewhat counterintuitive result, is found to be fully consistent with recent theoretical work. Grounding lines on retrograde slopes are conditionally stable, and the stability regime is a non-trivial function of bed and ice-shelf geometry. The stability of grounding lines cannot be assessed from considerations of local bed slope only. Text Ice Shelf Copernicus Publications: E-Journals The Cryosphere 7 2 647 655
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ice-shelf buttressing and the stability of marine-type ice sheets are investigated numerically. Buttressing effects are analysed for a situation where a stable grounding line is located on a bed sloping upwards in the direction of flow. Such grounding-line positions are known to be unconditionally unstable in the absence of transverse flow variations. It is shown that ice-shelf buttressing can restore stability under these conditions. Ice flux at the grounding line is, in general, not a monotonically increasing function of ice thickness. This, possibly at first somewhat counterintuitive result, is found to be fully consistent with recent theoretical work. Grounding lines on retrograde slopes are conditionally stable, and the stability regime is a non-trivial function of bed and ice-shelf geometry. The stability of grounding lines cannot be assessed from considerations of local bed slope only.
format Text
author Gudmundsson, G. H.
spellingShingle Gudmundsson, G. H.
Ice-shelf buttressing and the stability of marine ice sheets
author_facet Gudmundsson, G. H.
author_sort Gudmundsson, G. H.
title Ice-shelf buttressing and the stability of marine ice sheets
title_short Ice-shelf buttressing and the stability of marine ice sheets
title_full Ice-shelf buttressing and the stability of marine ice sheets
title_fullStr Ice-shelf buttressing and the stability of marine ice sheets
title_full_unstemmed Ice-shelf buttressing and the stability of marine ice sheets
title_sort ice-shelf buttressing and the stability of marine ice sheets
publishDate 2018
url https://doi.org/10.5194/tc-7-647-2013
https://tc.copernicus.org/articles/7/647/2013/
genre Ice Shelf
genre_facet Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-7-647-2013
https://tc.copernicus.org/articles/7/647/2013/
op_doi https://doi.org/10.5194/tc-7-647-2013
container_title The Cryosphere
container_volume 7
container_issue 2
container_start_page 647
op_container_end_page 655
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