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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Cambridge University Press (CUP)
1975
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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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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 |
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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 |
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15 |
container_issue |
73 |
container_start_page |
417 |
op_container_end_page |
427 |
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1792499616259768320 |