Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate

Abstract An analysis of records of annual mean temperatures around Antarctica shows large-scale anomalies of thousands of kilometers extent with typical variations of a deg from one year to another From 1967 on, composite satellite photographs are available which show considerable variation in the s...

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Published in:Journal of Glaciology
Main Author: Budd, W. F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000034523
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034523
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spelling crcambridgeupr:10.1017/s0022143000034523 2024-03-03T08:37:33+00:00 Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate Budd, W. F. 1975 http://dx.doi.org/10.1017/s0022143000034523 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034523 en eng Cambridge University Press (CUP) Journal of Glaciology volume 15, issue 73, page 417-427 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000034523 2024-02-08T08:37:11Z Abstract An analysis of records of annual mean temperatures around Antarctica shows large-scale anomalies of thousands of kilometers extent with typical variations of a deg from one year to another From 1967 on, composite satellite photographs are available which show considerable variation in the sea-ice extent in different years up to about 5º of latitude. These largest differences seem to persist over entire seasons. In general there seems to be considerable association between the region around the Antarctic with the coldest temperatures and the regions of greatest sea-ice extent. An analysis of long-term records at a single location near the edge of the Antarctic sea ice indicates a strong correlation between variations in the annual mean temperature and the duration of the sea ice, such that a change of 1 deg in the annual mean temperature corresponds to about 70 d variation in the duration of the sea ice. A relation is obtained between variations of annual mean temperature and the mean extent of the sea ice, viz. a 1 deg change corresponds to approximately 2.5º latitude variation in the maximum sea-ice extent. The magnitude of the variations in the sea-ice extent observed from the satellite data in comparison with the large-scale temperature anomalies is compatible with the above relations, although some rotational shifts appear to take place. Article in Journal/Newspaper Antarc* Antarctic Antarctica Journal of Glaciology Sea ice Cambridge University Press Antarctic The Antarctic Journal of Glaciology 15 73 417 427
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Budd, W. F.
Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
topic_facet Earth-Surface Processes
description Abstract An analysis of records of annual mean temperatures around Antarctica shows large-scale anomalies of thousands of kilometers extent with typical variations of a deg from one year to another From 1967 on, composite satellite photographs are available which show considerable variation in the sea-ice extent in different years up to about 5º of latitude. These largest differences seem to persist over entire seasons. In general there seems to be considerable association between the region around the Antarctic with the coldest temperatures and the regions of greatest sea-ice extent. An analysis of long-term records at a single location near the edge of the Antarctic sea ice indicates a strong correlation between variations in the annual mean temperature and the duration of the sea ice, such that a change of 1 deg in the annual mean temperature corresponds to about 70 d variation in the duration of the sea ice. A relation is obtained between variations of annual mean temperature and the mean extent of the sea ice, viz. a 1 deg change corresponds to approximately 2.5º latitude variation in the maximum sea-ice extent. The magnitude of the variations in the sea-ice extent observed from the satellite data in comparison with the large-scale temperature anomalies is compatible with the above relations, although some rotational shifts appear to take place.
format Article in Journal/Newspaper
author Budd, W. F.
author_facet Budd, W. F.
author_sort Budd, W. F.
title Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
title_short Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
title_full Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
title_fullStr Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
title_full_unstemmed Antarctic Sea-Ice Variations from Satellite Sensing in Relation to Climate
title_sort antarctic sea-ice variations from satellite sensing in relation to climate
publisher Cambridge University Press (CUP)
publishDate 1975
url http://dx.doi.org/10.1017/s0022143000034523
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034523
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Journal of Glaciology
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Journal of Glaciology
Sea ice
op_source Journal of Glaciology
volume 15, issue 73, page 417-427
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000034523
container_title Journal of Glaciology
container_volume 15
container_issue 73
container_start_page 417
op_container_end_page 427
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