Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment
Results are presented from the first investigation into a summer-season of mesoscale vortex activity in a large sector of the Antarctic coastal region. The study is based on an analysis of 3 months' meteorological satellite imagery collected at the British Research Station ‘Rothera’ on the Anta...
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Online Access: | http://nora.nerc.ac.uk/id/eprint/517520/ https://doi.org/10.1002/joc.3370140805 |
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ftnerc:oai:nora.nerc.ac.uk:517520 2023-05-15T13:49:34+02:00 Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment Turner, John Thomas, Jeremy P. 1994-10 http://nora.nerc.ac.uk/id/eprint/517520/ https://doi.org/10.1002/joc.3370140805 unknown Wiley Turner, John orcid:0000-0002-6111-5122 Thomas, Jeremy P. 1994 Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment. International Journal of Climatology, 14 (8). 871-894. https://doi.org/10.1002/joc.3370140805 <https://doi.org/10.1002/joc.3370140805> Atmospheric Sciences Publication - Article PeerReviewed 1994 ftnerc https://doi.org/10.1002/joc.3370140805 2023-02-04T19:45:13Z Results are presented from the first investigation into a summer-season of mesoscale vortex activity in a large sector of the Antarctic coastal region. The study is based on an analysis of 3 months' meteorological satellite imagery collected at the British Research Station ‘Rothera’ on the Antarctic Peninsula. The study revealed the high frequency with which such systems occur, with 162 individual vortices being found during the period December 1983 to February 1984 inclusive. The preferred area for their development was in the latitude band 60–70°S over the marginal ice zone and ice-free region of the eastern Bellingshausen Sea. A classification scheme for the vortices was developed based on the relationship with the broad-scale synoptic flow, the sea ice, and the geographical location. The most common type of vortex found was the ‘classic’ polar low, which formed in the southerly flow to the west of synoptic-scale disturbances. These vortices were very similar to the baroclinic type of polar lows observed south of Iceland during the Northern Hemisphere winter. A third of the vortices in total were found to be mesoscale features associated with synoptic-scale troughs or the centres of major depressions. Vortices with comma-shaped cloud signatures occurred about twice as frequently as those with spiraliform cloud. The vast majority of vortices had a diameter of less than 500 km, with very few systems being observed in the range 500–1000 km. Mean anomalies of 500 hPa geopotential height and surface pressure for the occasions when vortices were identified were —5.3 dm and — 0.5 hPa, respectively, indicating the association of these systems with upper air troughs and cold pools. Only 23 of the vortices found were correctly represented on the Meteorological Office analyses and of these 15 were small synoptic disturbances. The ‘polar low’ class of vortex was very poorly represented in the analyses, indicating that the available satellite sounder data could not resolve the systems and that the processes resulting in ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Iceland Sea ice Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Rothera ENVELOPE(-68.130,-68.130,-67.568,-67.568) International Journal of Climatology 14 8 871 894 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
topic |
Atmospheric Sciences |
spellingShingle |
Atmospheric Sciences Turner, John Thomas, Jeremy P. Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
topic_facet |
Atmospheric Sciences |
description |
Results are presented from the first investigation into a summer-season of mesoscale vortex activity in a large sector of the Antarctic coastal region. The study is based on an analysis of 3 months' meteorological satellite imagery collected at the British Research Station ‘Rothera’ on the Antarctic Peninsula. The study revealed the high frequency with which such systems occur, with 162 individual vortices being found during the period December 1983 to February 1984 inclusive. The preferred area for their development was in the latitude band 60–70°S over the marginal ice zone and ice-free region of the eastern Bellingshausen Sea. A classification scheme for the vortices was developed based on the relationship with the broad-scale synoptic flow, the sea ice, and the geographical location. The most common type of vortex found was the ‘classic’ polar low, which formed in the southerly flow to the west of synoptic-scale disturbances. These vortices were very similar to the baroclinic type of polar lows observed south of Iceland during the Northern Hemisphere winter. A third of the vortices in total were found to be mesoscale features associated with synoptic-scale troughs or the centres of major depressions. Vortices with comma-shaped cloud signatures occurred about twice as frequently as those with spiraliform cloud. The vast majority of vortices had a diameter of less than 500 km, with very few systems being observed in the range 500–1000 km. Mean anomalies of 500 hPa geopotential height and surface pressure for the occasions when vortices were identified were —5.3 dm and — 0.5 hPa, respectively, indicating the association of these systems with upper air troughs and cold pools. Only 23 of the vortices found were correctly represented on the Meteorological Office analyses and of these 15 were small synoptic disturbances. The ‘polar low’ class of vortex was very poorly represented in the analyses, indicating that the available satellite sounder data could not resolve the systems and that the processes resulting in ... |
format |
Article in Journal/Newspaper |
author |
Turner, John Thomas, Jeremy P. |
author_facet |
Turner, John Thomas, Jeremy P. |
author_sort |
Turner, John |
title |
Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
title_short |
Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
title_full |
Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
title_fullStr |
Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
title_full_unstemmed |
Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
title_sort |
summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment |
publisher |
Wiley |
publishDate |
1994 |
url |
http://nora.nerc.ac.uk/id/eprint/517520/ https://doi.org/10.1002/joc.3370140805 |
long_lat |
ENVELOPE(-68.130,-68.130,-67.568,-67.568) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Rothera |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Bellingshausen Sea Weddell Rothera |
genre |
Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Iceland Sea ice |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Iceland Sea ice |
op_relation |
Turner, John orcid:0000-0002-6111-5122 Thomas, Jeremy P. 1994 Summer-season mesoscale cyclones in the bellingshausen-weddell region of the antarctic and links with the synoptic-scale environment. International Journal of Climatology, 14 (8). 871-894. https://doi.org/10.1002/joc.3370140805 <https://doi.org/10.1002/joc.3370140805> |
op_doi |
https://doi.org/10.1002/joc.3370140805 |
container_title |
International Journal of Climatology |
container_volume |
14 |
container_issue |
8 |
container_start_page |
871 |
op_container_end_page |
894 |
_version_ |
1766251675127906304 |