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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2016-01-01
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Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/10/1/2016/tc-10-1-2016.pdf |
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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 |
work_keys_str_mv |
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