Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989.
The synoptic and mesoscale meteorological conditions were analyzed for Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. Meteorological observations from a research ship (R/V Polarbjoern), an array of drifting buoys and satellite imagery from DMS...
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Monterey, California. Naval Postgraduate School
1991
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ftnavalpschool:oai:calhoun.nps.edu:10945/26627 2024-06-09T07:42:53+00:00 Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. Hamilton, Stephanie W. Davidson, Kenneth L. Wash, Carlyle H. Naval Postgraduate School Meteorology Physical Oceanography 1991-03 87 p.;28 cm. application/pdf https://hdl.handle.net/10945/26627 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/26627 arctic meteorology arctic storms arctic climate arctic research boundary layer front marginal ice zone CEAREX Thesis 1991 ftnavalpschool 2024-05-15T01:00:01Z The synoptic and mesoscale meteorological conditions were analyzed for Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. Meteorological observations from a research ship (R/V Polarbjoern), an array of drifting buoys and satellite imagery from DMSP and NOAA satellites were the primary tools for analysis. Several short periods of high cyclone activity followed by long periods of high pressure dominated the weather pattern in the eastern Arctic Ocean from Greenland to Novaya Zemlya for this period. Two case studies are presented. An infrequent cyclogenesis event that formed within a strong baroclinic zone over Arctic pack ice was observed in a "baroclinic leaf on satellite imagery. Ship and drifting buoy observations provided critical insight to the location and intensity of the "leafs" subsequent vertical development to the surface. In the second study, a boundary layer front was observed in the East Greenland Sea by satellite imagery. The front then moved northeast into Fram Strait and a polar low formed at the northern end of the front. The event lasted less than 24 h and would not have been observed except through satellite imagery. Lieutenant, United States Navy http://archive.org/details/meteorologicalfe1094526627 Thesis Arctic Arctic Ocean East Greenland Fram Strait Greenland Greenland Sea Novaya Zemlya Naval Postgraduate School: Calhoun Arctic Arctic Ocean Greenland |
institution |
Open Polar |
collection |
Naval Postgraduate School: Calhoun |
op_collection_id |
ftnavalpschool |
language |
English |
topic |
arctic meteorology arctic storms arctic climate arctic research boundary layer front marginal ice zone CEAREX |
spellingShingle |
arctic meteorology arctic storms arctic climate arctic research boundary layer front marginal ice zone CEAREX Hamilton, Stephanie W. Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
topic_facet |
arctic meteorology arctic storms arctic climate arctic research boundary layer front marginal ice zone CEAREX |
description |
The synoptic and mesoscale meteorological conditions were analyzed for Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. Meteorological observations from a research ship (R/V Polarbjoern), an array of drifting buoys and satellite imagery from DMSP and NOAA satellites were the primary tools for analysis. Several short periods of high cyclone activity followed by long periods of high pressure dominated the weather pattern in the eastern Arctic Ocean from Greenland to Novaya Zemlya for this period. Two case studies are presented. An infrequent cyclogenesis event that formed within a strong baroclinic zone over Arctic pack ice was observed in a "baroclinic leaf on satellite imagery. Ship and drifting buoy observations provided critical insight to the location and intensity of the "leafs" subsequent vertical development to the surface. In the second study, a boundary layer front was observed in the East Greenland Sea by satellite imagery. The front then moved northeast into Fram Strait and a polar low formed at the northern end of the front. The event lasted less than 24 h and would not have been observed except through satellite imagery. Lieutenant, United States Navy http://archive.org/details/meteorologicalfe1094526627 |
author2 |
Davidson, Kenneth L. Wash, Carlyle H. Naval Postgraduate School Meteorology Physical Oceanography |
format |
Thesis |
author |
Hamilton, Stephanie W. |
author_facet |
Hamilton, Stephanie W. |
author_sort |
Hamilton, Stephanie W. |
title |
Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
title_short |
Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
title_full |
Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
title_fullStr |
Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
title_full_unstemmed |
Meteorological features during Phase I of the Coordinated Eastern Arctic Experiment (CEAREX) from 17 September 1988 to 7 January 1989. |
title_sort |
meteorological features during phase i of the coordinated eastern arctic experiment (cearex) from 17 september 1988 to 7 january 1989. |
publisher |
Monterey, California. Naval Postgraduate School |
publishDate |
1991 |
url |
https://hdl.handle.net/10945/26627 |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Arctic Arctic Ocean East Greenland Fram Strait Greenland Greenland Sea Novaya Zemlya |
genre_facet |
Arctic Arctic Ocean East Greenland Fram Strait Greenland Greenland Sea Novaya Zemlya |
op_relation |
https://hdl.handle.net/10945/26627 |
_version_ |
1801371583212683264 |