A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets

Predicting the evolution of ice sheets requires numerical models able to accurately track the migration of ice sheet continental margins or grounding lines. We introduce a physically based moving-point approach for the flow of ice sheets based on the conservation of local masses. This allows the ice...

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Main Authors: B. Bonan, M. J. Baines, N. K. Nichols, D. Partridge
Format: Article
Language:English
Published: Copernicus Publications 2016-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/10/1/2016/tc-10-1-2016.pdf
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spelling doaj-870f690fe6764a689a0a810e7f77356b2020-11-24T21:04:21ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242016-01-0110111410.5194/tc-10-1-2016A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheetsB. Bonan0M. J. Baines1N. K. Nichols2D. Partridge3School of Mathematical and Physical Sciences, University of Reading, Reading, UKSchool of Mathematical and Physical Sciences, University of Reading, Reading, UKSchool of Mathematical and Physical Sciences, University of Reading, Reading, UKSchool of Mathematical and Physical Sciences, University of Reading, Reading, UKPredicting the evolution of ice sheets requires numerical models able to accurately track the migration of ice sheet continental margins or grounding lines. We introduce a physically based moving-point approach for the flow of ice sheets based on the conservation of local masses. This allows the ice sheet margins to be tracked explicitly. Our approach is also well suited to capture waiting-time behaviour efficiently. A finite-difference moving-point scheme is derived and applied in a simplified context (continental radially symmetrical shallow ice approximation). The scheme, which is inexpensive, is verified by comparing the results with steady states obtained from an analytic solution and with exact moving-margin transient solutions. In both cases the scheme is able to track the position of the ice sheet margin with high accuracy.http://www.the-cryosphere.net/10/1/2016/tc-10-1-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Bonan
M. J. Baines
N. K. Nichols
D. Partridge
spellingShingle B. Bonan
M. J. Baines
N. K. Nichols
D. Partridge
A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
The Cryosphere
author_facet B. Bonan
M. J. Baines
N. K. Nichols
D. Partridge
author_sort B. Bonan
title A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
title_short A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
title_full A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
title_fullStr A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
title_full_unstemmed A moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
title_sort moving-point approach to model shallow ice sheets: a study case with radially symmetrical ice sheets
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2016-01-01
description Predicting the evolution of ice sheets requires numerical models able to accurately track the migration of ice sheet continental margins or grounding lines. We introduce a physically based moving-point approach for the flow of ice sheets based on the conservation of local masses. This allows the ice sheet margins to be tracked explicitly. Our approach is also well suited to capture waiting-time behaviour efficiently. A finite-difference moving-point scheme is derived and applied in a simplified context (continental radially symmetrical shallow ice approximation). The scheme, which is inexpensive, is verified by comparing the results with steady states obtained from an analytic solution and with exact moving-margin transient solutions. In both cases the scheme is able to track the position of the ice sheet margin with high accuracy.
url http://www.the-cryosphere.net/10/1/2016/tc-10-1-2016.pdf
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