Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula

Summary An analysis of changes of atmospheric circulation in the Southern Hemisphere in relation to recent warming at the Antarctic Peninsula in last thirty years is presented. The sea level pressure and geopotential fields change in 1960-2000 are considered. It was shown that large-scale baric form...

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Main Authors: V. Martazinova, V. Tymofeyev
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.9068
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.519.9068 2023-05-15T14:02:35+02:00 Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula V. Martazinova V. Tymofeyev The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.9068 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.9068 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf text ftciteseerx 2016-01-08T10:02:21Z Summary An analysis of changes of atmospheric circulation in the Southern Hemisphere in relation to recent warming at the Antarctic Peninsula in last thirty years is presented. The sea level pressure and geopotential fields change in 1960-2000 are considered. It was shown that large-scale baric formations of the Southern Hemisphere had displaced to the west about 15-20o during this period. It resulted in the warm winters in last years at the Antarctic Peninsula region. The approach to the classification of meteorological fields based on the method of analogs of synoptic processes (etalon-field method) is briefly described and applied to extra tropical sector of Southern Hemisphere that includes Antarctic. The most informative ‘etalon ’ weather patterns were set off for each decade 1960-2000. Predominant weather pattern in 1990s shows more intensive cyclonicity, with series of cyclones west of the Antarctic Peninsula, and depression at the Bellingshausen Sea in the place of the ridge in 1960s. Citation: Martazinova V., Tymofeyev V. (2007), Recent warming at the Antarctic Peninsula as viewed against changes in atmospheric circulation,in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES X, edited by A. K. Cooper and C. R. Raymond et al., USGS Text Antarc* Antarctic Antarctic Peninsula Antarctica Bellingshausen Sea Unknown Antarctic Antarctic Peninsula Bellingshausen Sea The Antarctic
institution Open Polar
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op_collection_id ftciteseerx
language English
description Summary An analysis of changes of atmospheric circulation in the Southern Hemisphere in relation to recent warming at the Antarctic Peninsula in last thirty years is presented. The sea level pressure and geopotential fields change in 1960-2000 are considered. It was shown that large-scale baric formations of the Southern Hemisphere had displaced to the west about 15-20o during this period. It resulted in the warm winters in last years at the Antarctic Peninsula region. The approach to the classification of meteorological fields based on the method of analogs of synoptic processes (etalon-field method) is briefly described and applied to extra tropical sector of Southern Hemisphere that includes Antarctic. The most informative ‘etalon ’ weather patterns were set off for each decade 1960-2000. Predominant weather pattern in 1990s shows more intensive cyclonicity, with series of cyclones west of the Antarctic Peninsula, and depression at the Bellingshausen Sea in the place of the ridge in 1960s. Citation: Martazinova V., Tymofeyev V. (2007), Recent warming at the Antarctic Peninsula as viewed against changes in atmospheric circulation,in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES X, edited by A. K. Cooper and C. R. Raymond et al., USGS
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author V. Martazinova
V. Tymofeyev
spellingShingle V. Martazinova
V. Tymofeyev
Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
author_facet V. Martazinova
V. Tymofeyev
author_sort V. Martazinova
title Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
title_short Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
title_full Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
title_fullStr Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
title_full_unstemmed Interdecadal changes of tropospheric circulation in Southern extratropics during the recent warming in the Antarctic Peninsula
title_sort interdecadal changes of tropospheric circulation in southern extratropics during the recent warming in the antarctic peninsula
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.9068
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf
geographic Antarctic
Antarctic Peninsula
Bellingshausen Sea
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Bellingshausen Sea
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Bellingshausen Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Bellingshausen Sea
op_source http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.9068
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea067.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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