Heat Conduction in Thinning Ice Sheets

Abstract A numerical treatment of the heat conduction in ice sheets subject to vertical shrinking, geothermal and frictional heating from below, and surface accumulation or ablation, is outlined and illustrated with results computed for an arbitrary ice thickness profile. The movement of the ice is...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Jenssen, D., Radok, U.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1963
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000027817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027817
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spelling crcambridgeupr:10.1017/s0022143000027817 2024-03-03T08:45:58+00:00 Heat Conduction in Thinning Ice Sheets Jenssen, D. Radok, U. 1963 http://dx.doi.org/10.1017/s0022143000027817 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027817 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 34, page 387-397 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1963 crcambridgeupr https://doi.org/10.1017/s0022143000027817 2024-02-08T08:42:50Z Abstract A numerical treatment of the heat conduction in ice sheets subject to vertical shrinking, geothermal and frictional heating from below, and surface accumulation or ablation, is outlined and illustrated with results computed for an arbitrary ice thickness profile. The movement of the ice is found to increase its basal temperature when the ice is thick, and to decrease it in the fringe zone where the ice becomes thin. The treatment seems capable of extension to cover both the thermal and dynamic aspects of ice motion. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 4 34 387 397
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Jenssen, D.
Radok, U.
Heat Conduction in Thinning Ice Sheets
topic_facet Earth-Surface Processes
description Abstract A numerical treatment of the heat conduction in ice sheets subject to vertical shrinking, geothermal and frictional heating from below, and surface accumulation or ablation, is outlined and illustrated with results computed for an arbitrary ice thickness profile. The movement of the ice is found to increase its basal temperature when the ice is thick, and to decrease it in the fringe zone where the ice becomes thin. The treatment seems capable of extension to cover both the thermal and dynamic aspects of ice motion.
format Article in Journal/Newspaper
author Jenssen, D.
Radok, U.
author_facet Jenssen, D.
Radok, U.
author_sort Jenssen, D.
title Heat Conduction in Thinning Ice Sheets
title_short Heat Conduction in Thinning Ice Sheets
title_full Heat Conduction in Thinning Ice Sheets
title_fullStr Heat Conduction in Thinning Ice Sheets
title_full_unstemmed Heat Conduction in Thinning Ice Sheets
title_sort heat conduction in thinning ice sheets
publisher Cambridge University Press (CUP)
publishDate 1963
url http://dx.doi.org/10.1017/s0022143000027817
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000027817
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 4, issue 34, page 387-397
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000027817
container_title Journal of Glaciology
container_volume 4
container_issue 34
container_start_page 387
op_container_end_page 397
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