Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet

The shallow ice approximation (SIA) is commonly used in ice-sheet models to simplify the force balance equations within the ice. However, the SIA cannot adequately reproduce the dynamics of the fast flowing ice streams usually found at the margins of ice sheets. To overcome this limitation, recent s...

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Published in:The Cryosphere
Main Authors: J. Bernales, I. Rogozhina, R. Greve, M. Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-11-247-2017
http://www.the-cryosphere.net/11/247/2017/tc-11-247-2017.pdf
https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:bab29ded91304a8da282d02b6ca4bb31 2023-05-15T13:39:35+02:00 Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet J. Bernales I. Rogozhina R. Greve M. Thomas 2017-01-01 https://doi.org/10.5194/tc-11-247-2017 http://www.the-cryosphere.net/11/247/2017/tc-11-247-2017.pdf https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-11-247-2017 http://www.the-cryosphere.net/11/247/2017/tc-11-247-2017.pdf https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31 undefined The Cryosphere, Vol 11, Iss 1, Pp 247-265 (2017) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2017 fttriple https://doi.org/10.5194/tc-11-247-2017 2023-01-22T18:19:38Z The shallow ice approximation (SIA) is commonly used in ice-sheet models to simplify the force balance equations within the ice. However, the SIA cannot adequately reproduce the dynamics of the fast flowing ice streams usually found at the margins of ice sheets. To overcome this limitation, recent studies have introduced heuristic hybrid combinations of the SIA and the shelfy stream approximation. Here, we implement four different hybrid schemes into a model of the Antarctic Ice Sheet in order to compare their performance under present-day conditions. For each scheme, the model is calibrated using an iterative technique to infer the spatial variability in basal sliding parameters. Model results are validated against topographic and velocity data. Our analysis shows that the iterative technique compensates for the differences between the schemes, producing similar ice-sheet configurations through quantitatively different results of the sliding coefficient calibration. Despite this we observe a robust agreement in the reconstructed patterns of basal sliding parameters. We exchange the calibrated sliding parameter distributions between the schemes to demonstrate that the results of the model calibration cannot be straightforwardly transferred to models based on different approximations of ice dynamics. However, easily adaptable calibration techniques for the potential distribution of basal sliding coefficients can be implemented into ice models to overcome such incompatibility, as shown in this study. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet The Cryosphere Unknown Antarctic The Antarctic The Cryosphere 11 1 247 265
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
J. Bernales
I. Rogozhina
R. Greve
M. Thomas
Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
topic_facet geo
envir
description The shallow ice approximation (SIA) is commonly used in ice-sheet models to simplify the force balance equations within the ice. However, the SIA cannot adequately reproduce the dynamics of the fast flowing ice streams usually found at the margins of ice sheets. To overcome this limitation, recent studies have introduced heuristic hybrid combinations of the SIA and the shelfy stream approximation. Here, we implement four different hybrid schemes into a model of the Antarctic Ice Sheet in order to compare their performance under present-day conditions. For each scheme, the model is calibrated using an iterative technique to infer the spatial variability in basal sliding parameters. Model results are validated against topographic and velocity data. Our analysis shows that the iterative technique compensates for the differences between the schemes, producing similar ice-sheet configurations through quantitatively different results of the sliding coefficient calibration. Despite this we observe a robust agreement in the reconstructed patterns of basal sliding parameters. We exchange the calibrated sliding parameter distributions between the schemes to demonstrate that the results of the model calibration cannot be straightforwardly transferred to models based on different approximations of ice dynamics. However, easily adaptable calibration techniques for the potential distribution of basal sliding coefficients can be implemented into ice models to overcome such incompatibility, as shown in this study.
format Article in Journal/Newspaper
author J. Bernales
I. Rogozhina
R. Greve
M. Thomas
author_facet J. Bernales
I. Rogozhina
R. Greve
M. Thomas
author_sort J. Bernales
title Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
title_short Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
title_full Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
title_fullStr Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
title_full_unstemmed Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
title_sort comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the antarctic ice sheet
publisher Copernicus Publications
publishDate 2017
url https://doi.org/10.5194/tc-11-247-2017
http://www.the-cryosphere.net/11/247/2017/tc-11-247-2017.pdf
https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
The Cryosphere
genre_facet Antarc*
Antarctic
Ice Sheet
The Cryosphere
op_source The Cryosphere, Vol 11, Iss 1, Pp 247-265 (2017)
op_relation 1994-0416
1994-0424
doi:10.5194/tc-11-247-2017
http://www.the-cryosphere.net/11/247/2017/tc-11-247-2017.pdf
https://doaj.org/article/bab29ded91304a8da282d02b6ca4bb31
op_rights undefined
op_doi https://doi.org/10.5194/tc-11-247-2017
container_title The Cryosphere
container_volume 11
container_issue 1
container_start_page 247
op_container_end_page 265
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