The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream
An atmospheric general circulation model with prescribed sea-ice and sea-surface temperatures is used to examine the sensitivity of the atmospheric circulation to changes in sea-ice extent in the Southern Hemisphere. Experiments are conducted where the sea-ice edge is expanded or contracted by 7 deg...
Published in: | Geophysical Research Letters |
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American Geophysical Union
2011
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Online Access: | http://hdl.handle.net/1959.4/unsworks_41960 https://doi.org/10.1029/2011GL048056 |
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ftunswworks:oai:unsworks.library.unsw.edu.au:1959.4/unsworks_41960 2024-06-02T07:58:04+00:00 The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream Kidston, J Taschetto, AS Thompson, DWJ England, MH 2011 http://hdl.handle.net/1959.4/unsworks_41960 https://doi.org/10.1029/2011GL048056 unknown American Geophysical Union http://purl.org/au-research/grants/arc/FL100100214 http://hdl.handle.net/1959.4/unsworks_41960 https://doi.org/10.1029/2011GL048056 metadata only access http://purl.org/coar/access_right/c_14cb CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ urn:ISSN:0094-8276 urn:ISSN:1944-8007 Geophysical Research Letters, 38, 15, L15804 journal article http://purl.org/coar/resource_type/c_6501 2011 ftunswworks https://doi.org/10.1029/2011GL048056 2024-05-07T23:52:49Z An atmospheric general circulation model with prescribed sea-ice and sea-surface temperatures is used to examine the sensitivity of the atmospheric circulation to changes in sea-ice extent in the Southern Hemisphere. Experiments are conducted where the sea-ice edge is expanded or contracted by 7 degrees of latitude compared with its position in a control run. The experiments suggest that the latitude of the sea-ice edge influences the latitude of the Southern Hemisphere mid-latitude jet stream, but that the amplitude of the atmospheric response depends critically on the location and seasonality of the sea-ice anomalies. During the cold season, the mid-latitude jet shifts significantly poleward when the sea-ice extent is increased, but exhibits very little response when the sea-ice extent is decreased. During the warm season, the jet does not shift significantly regardless of whether the sea-ice edge is extended or contracted. The cause of the asymmetry in the atmospheric response relates to the extent to which the sea-ice anomalies affect meridional temperature gradients in the near-surface baroclinic zone. The results suggest that 1) any future decreases in Antarctic sea-ice are unlikely to have a profound effect on the Southern Hemisphere mid-latitude circulation; and 2) the usefulness of sea-ice variability for seasonal prediction is limited to the cold season and to the case of increases in sea-ice extent. Article in Journal/Newspaper Antarc* Antarctic Sea ice UNSW Sydney (The University of New South Wales): UNSWorks Antarctic Geophysical Research Letters 38 15 |
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Open Polar |
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UNSW Sydney (The University of New South Wales): UNSWorks |
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ftunswworks |
language |
unknown |
description |
An atmospheric general circulation model with prescribed sea-ice and sea-surface temperatures is used to examine the sensitivity of the atmospheric circulation to changes in sea-ice extent in the Southern Hemisphere. Experiments are conducted where the sea-ice edge is expanded or contracted by 7 degrees of latitude compared with its position in a control run. The experiments suggest that the latitude of the sea-ice edge influences the latitude of the Southern Hemisphere mid-latitude jet stream, but that the amplitude of the atmospheric response depends critically on the location and seasonality of the sea-ice anomalies. During the cold season, the mid-latitude jet shifts significantly poleward when the sea-ice extent is increased, but exhibits very little response when the sea-ice extent is decreased. During the warm season, the jet does not shift significantly regardless of whether the sea-ice edge is extended or contracted. The cause of the asymmetry in the atmospheric response relates to the extent to which the sea-ice anomalies affect meridional temperature gradients in the near-surface baroclinic zone. The results suggest that 1) any future decreases in Antarctic sea-ice are unlikely to have a profound effect on the Southern Hemisphere mid-latitude circulation; and 2) the usefulness of sea-ice variability for seasonal prediction is limited to the cold season and to the case of increases in sea-ice extent. |
format |
Article in Journal/Newspaper |
author |
Kidston, J Taschetto, AS Thompson, DWJ England, MH |
spellingShingle |
Kidston, J Taschetto, AS Thompson, DWJ England, MH The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
author_facet |
Kidston, J Taschetto, AS Thompson, DWJ England, MH |
author_sort |
Kidston, J |
title |
The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
title_short |
The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
title_full |
The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
title_fullStr |
The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
title_full_unstemmed |
The influence of Southern Hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
title_sort |
influence of southern hemisphere sea-ice extent on the latitude of the mid-latitude jet stream |
publisher |
American Geophysical Union |
publishDate |
2011 |
url |
http://hdl.handle.net/1959.4/unsworks_41960 https://doi.org/10.1029/2011GL048056 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_source |
urn:ISSN:0094-8276 urn:ISSN:1944-8007 Geophysical Research Letters, 38, 15, L15804 |
op_relation |
http://purl.org/au-research/grants/arc/FL100100214 http://hdl.handle.net/1959.4/unsworks_41960 https://doi.org/10.1029/2011GL048056 |
op_rights |
metadata only access http://purl.org/coar/access_right/c_14cb CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ |
op_doi |
https://doi.org/10.1029/2011GL048056 |
container_title |
Geophysical Research Letters |
container_volume |
38 |
container_issue |
15 |
_version_ |
1800741328403824640 |