On the Response of a Sea-Ice Cover to Changes in Surface Temperature

The time separation between related extremes in the values of surface temperature and growth rate of a floating ice cover are shown to depend on the mean ice temperature and thickness. A quantity termed the lag coefficient is introduced for which observations from Churchill, Hudson Bay, and Davis, A...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Schwerdtfeger, Peter
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1966
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000019560
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019560
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spelling crcambridgeupr:10.1017/s0022143000019560 2024-03-03T08:38:59+00:00 On the Response of a Sea-Ice Cover to Changes in Surface Temperature Schwerdtfeger, Peter 1966 http://dx.doi.org/10.1017/s0022143000019560 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019560 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 45, page 439-442 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1966 crcambridgeupr https://doi.org/10.1017/s0022143000019560 2024-02-08T08:41:37Z The time separation between related extremes in the values of surface temperature and growth rate of a floating ice cover are shown to depend on the mean ice temperature and thickness. A quantity termed the lag coefficient is introduced for which observations from Churchill, Hudson Bay, and Davis, Antarctica, suggest a dependence on temperature but not on geography. Article in Journal/Newspaper Antarc* Antarctica Hudson Bay Journal of Glaciology Sea ice Cambridge University Press Hudson Bay Hudson Journal of Glaciology 6 45 439 442
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Schwerdtfeger, Peter
On the Response of a Sea-Ice Cover to Changes in Surface Temperature
topic_facet Earth-Surface Processes
description The time separation between related extremes in the values of surface temperature and growth rate of a floating ice cover are shown to depend on the mean ice temperature and thickness. A quantity termed the lag coefficient is introduced for which observations from Churchill, Hudson Bay, and Davis, Antarctica, suggest a dependence on temperature but not on geography.
format Article in Journal/Newspaper
author Schwerdtfeger, Peter
author_facet Schwerdtfeger, Peter
author_sort Schwerdtfeger, Peter
title On the Response of a Sea-Ice Cover to Changes in Surface Temperature
title_short On the Response of a Sea-Ice Cover to Changes in Surface Temperature
title_full On the Response of a Sea-Ice Cover to Changes in Surface Temperature
title_fullStr On the Response of a Sea-Ice Cover to Changes in Surface Temperature
title_full_unstemmed On the Response of a Sea-Ice Cover to Changes in Surface Temperature
title_sort on the response of a sea-ice cover to changes in surface temperature
publisher Cambridge University Press (CUP)
publishDate 1966
url http://dx.doi.org/10.1017/s0022143000019560
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019560
geographic Hudson Bay
Hudson
geographic_facet Hudson Bay
Hudson
genre Antarc*
Antarctica
Hudson Bay
Journal of Glaciology
Sea ice
genre_facet Antarc*
Antarctica
Hudson Bay
Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 6, issue 45, page 439-442
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000019560
container_title Journal of Glaciology
container_volume 6
container_issue 45
container_start_page 439
op_container_end_page 442
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