A Thermohydrodynamic Model of an Ice Sheet
Abstract The purpose of this paper is to consider an ice-sheet model based on joint solution to the dynamic equations and equations of heat conductivity in which the surface relief is one of the unknown functions. The proposed model is applicable to calculations of the Antarctic ice sheet. Results o...
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Cambridge University Press (CUP)
1980
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Online Access: | http://dx.doi.org/10.1017/s0022143000010285 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010285 |
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crcambridgeupr:10.1017/s0022143000010285 2024-03-03T08:36:56+00:00 A Thermohydrodynamic Model of an Ice Sheet Verbitsky, M. Ya. Chalikov, D. V. 1980 http://dx.doi.org/10.1017/s0022143000010285 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010285 en eng Cambridge University Press (CUP) Journal of Glaciology volume 25, issue 91, page 61-68 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1980 crcambridgeupr https://doi.org/10.1017/s0022143000010285 2024-02-08T08:32:56Z Abstract The purpose of this paper is to consider an ice-sheet model based on joint solution to the dynamic equations and equations of heat conductivity in which the surface relief is one of the unknown functions. The proposed model is applicable to calculations of the Antarctic ice sheet. Results of a numerical experiment for present values of the temperature of the ice surface and precipitation as well as for their separate and simultaneous increase by 2, 4, or 6 deg and 10, 20, or 30% are given. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Journal of Glaciology Cambridge University Press Antarctic The Antarctic Journal of Glaciology 25 91 61 68 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Verbitsky, M. Ya. Chalikov, D. V. A Thermohydrodynamic Model of an Ice Sheet |
topic_facet |
Earth-Surface Processes |
description |
Abstract The purpose of this paper is to consider an ice-sheet model based on joint solution to the dynamic equations and equations of heat conductivity in which the surface relief is one of the unknown functions. The proposed model is applicable to calculations of the Antarctic ice sheet. Results of a numerical experiment for present values of the temperature of the ice surface and precipitation as well as for their separate and simultaneous increase by 2, 4, or 6 deg and 10, 20, or 30% are given. |
format |
Article in Journal/Newspaper |
author |
Verbitsky, M. Ya. Chalikov, D. V. |
author_facet |
Verbitsky, M. Ya. Chalikov, D. V. |
author_sort |
Verbitsky, M. Ya. |
title |
A Thermohydrodynamic Model of an Ice Sheet |
title_short |
A Thermohydrodynamic Model of an Ice Sheet |
title_full |
A Thermohydrodynamic Model of an Ice Sheet |
title_fullStr |
A Thermohydrodynamic Model of an Ice Sheet |
title_full_unstemmed |
A Thermohydrodynamic Model of an Ice Sheet |
title_sort |
thermohydrodynamic model of an ice sheet |
publisher |
Cambridge University Press (CUP) |
publishDate |
1980 |
url |
http://dx.doi.org/10.1017/s0022143000010285 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000010285 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Ice Sheet Journal of Glaciology |
genre_facet |
Antarc* Antarctic Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 25, issue 91, page 61-68 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000010285 |
container_title |
Journal of Glaciology |
container_volume |
25 |
container_issue |
91 |
container_start_page |
61 |
op_container_end_page |
68 |
_version_ |
1792496464334684160 |