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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Published in:Journal of Glaciology
Main Authors: Verbitsky, M. Ya., Chalikov, D. V.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
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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spelling 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
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