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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Main Authors: Bernales, Jorge, Rogozhina, Irina, Greve, Ralf, Thomas, Maik
Format: Article in Journal/Newspaper
Language:unknown
Published: Freie Universität Berlin 2017
Subjects:
Online Access:https://dx.doi.org/10.17169/refubium-24304
https://refubium.fu-berlin.de/handle/fub188/21007
id ftdatacite:10.17169/refubium-24304
record_format openpolar
spelling ftdatacite:10.17169/refubium-24304 2023-05-15T13:52:29+02:00 Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet Bernales, Jorge Rogozhina, Irina Greve, Ralf Thomas, Maik 2017 https://dx.doi.org/10.17169/refubium-24304 https://refubium.fu-berlin.de/handle/fub188/21007 unknown Freie Universität Berlin http://creativecommons.org/licenses/by/3.0 CC-BY 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie CreativeWork article 2017 ftdatacite https://doi.org/10.17169/refubium-24304 2021-11-05T12:55:41Z 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 DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie
spellingShingle 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie
Bernales, Jorge
Rogozhina, Irina
Greve, Ralf
Thomas, Maik
Comparison of hybrid schemes for the combination of shallow approximations in numerical simulations of the Antarctic Ice Sheet
topic_facet 500 Naturwissenschaften und Mathematik550 Geowissenschaften, Geologie
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 Bernales, Jorge
Rogozhina, Irina
Greve, Ralf
Thomas, Maik
author_facet Bernales, Jorge
Rogozhina, Irina
Greve, Ralf
Thomas, Maik
author_sort Bernales, Jorge
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 Freie Universität Berlin
publishDate 2017
url https://dx.doi.org/10.17169/refubium-24304
https://refubium.fu-berlin.de/handle/fub188/21007
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_rights http://creativecommons.org/licenses/by/3.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.17169/refubium-24304
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