Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets

Abstract Mass loss from ice shelves is a strong control on grounding-line dynamics. Here we investigate how calving and submarine melt parameterizations affect steady-state grounding-line positions and their stability. Our results indicate that different calving laws with the same melt parameterizat...

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Published in:Journal of Glaciology
Main Authors: Haseloff, Marianne, Sergienko, Olga V.
Other Authors: Northumbria University, National Oceanic and Atmospheric Administration
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.29
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000296
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spelling crcambridgeupr:10.1017/jog.2022.29 2024-06-23T07:53:49+00:00 Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets Haseloff, Marianne Sergienko, Olga V. Northumbria University National Oceanic and Atmospheric Administration 2022 http://dx.doi.org/10.1017/jog.2022.29 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000296 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 68, issue 272, page 1149-1166 ISSN 0022-1430 1727-5652 journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2022.29 2024-06-12T04:04:10Z Abstract Mass loss from ice shelves is a strong control on grounding-line dynamics. Here we investigate how calving and submarine melt parameterizations affect steady-state grounding-line positions and their stability. Our results indicate that different calving laws with the same melt parameterization result in more diverse steady-state ice-sheet configurations than different melt parameterizations with the same calving law. We show that the backstress at the grounding line depends on the integrated ice-shelf mass flux. Consequently, ice shelves are most sensitive to high melt rates in the vicinity of their grounding lines. For the same shelf-averaged melt rates, different melt parameterizations can lead to very different ice-shelf configurations and grounding-line positions. If the melt rate depends on the slope of the ice-shelf draft, then the positive feedback between increased melting and steepening of the slope can lead to singular melt rates at the ice-shelf front, producing an apparent lower limit of the shelf front thickness as the ice thickness vanishes over a small boundary layer. Our results illustrate that the evolution of marine ice sheets is highly dependent on ice-shelf mass loss mechanisms, and that existing parameterizations can lead to a wide range of modelled grounding-line behaviours. Article in Journal/Newspaper Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Cambridge University Press Journal of Glaciology 1 18
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Mass loss from ice shelves is a strong control on grounding-line dynamics. Here we investigate how calving and submarine melt parameterizations affect steady-state grounding-line positions and their stability. Our results indicate that different calving laws with the same melt parameterization result in more diverse steady-state ice-sheet configurations than different melt parameterizations with the same calving law. We show that the backstress at the grounding line depends on the integrated ice-shelf mass flux. Consequently, ice shelves are most sensitive to high melt rates in the vicinity of their grounding lines. For the same shelf-averaged melt rates, different melt parameterizations can lead to very different ice-shelf configurations and grounding-line positions. If the melt rate depends on the slope of the ice-shelf draft, then the positive feedback between increased melting and steepening of the slope can lead to singular melt rates at the ice-shelf front, producing an apparent lower limit of the shelf front thickness as the ice thickness vanishes over a small boundary layer. Our results illustrate that the evolution of marine ice sheets is highly dependent on ice-shelf mass loss mechanisms, and that existing parameterizations can lead to a wide range of modelled grounding-line behaviours.
author2 Northumbria University
National Oceanic and Atmospheric Administration
format Article in Journal/Newspaper
author Haseloff, Marianne
Sergienko, Olga V.
spellingShingle Haseloff, Marianne
Sergienko, Olga V.
Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
author_facet Haseloff, Marianne
Sergienko, Olga V.
author_sort Haseloff, Marianne
title Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
title_short Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
title_full Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
title_fullStr Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
title_full_unstemmed Effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
title_sort effects of calving and submarine melting on steady states and stability of buttressed marine ice sheets
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2022.29
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000296
genre Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
genre_facet Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
op_source Journal of Glaciology
volume 68, issue 272, page 1149-1166
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.29
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 18
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