Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone.
This thesis summarizes meteorological conditions occurring in the Marginal Ice Zone Experiment (MIZEX-84), conducted in the East Greenland Sea during the summer of 1984, are summarized. It includes a discussion of the synoptic and mesoscale conditions. The three cases discussed are: a weak storm whi...
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ftdtic:ADA165016 2023-05-15T14:57:48+02:00 Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. Phegley,Larry D NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1985-12 text/html http://www.dtic.mil/docs/citations/ADA165016 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA165016 en eng http://www.dtic.mil/docs/citations/ADA165016 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology Snow Ice and Permafrost *WEATHER *METEOROLOGICAL PHENOMENA *SEA ICE POLAR REGIONS COASTAL REGIONS INTENSITY THESES ICE STORMS NORTH(DIRECTION) LOW STRENGTH BASINS(GEOGRAPHIC) ARCTIC REGIONS GREENLAND SEA EAST(DIRECTION) GREENLAND STRAITS Marginal ice zone Text 1985 ftdtic 2016-02-21T01:32:39Z This thesis summarizes meteorological conditions occurring in the Marginal Ice Zone Experiment (MIZEX-84), conducted in the East Greenland Sea during the summer of 1984, are summarized. It includes a discussion of the synoptic and mesoscale conditions. The three cases discussed are: a weak storm which filled over the marginal ice zone (MIZ); an intense storm which transited the MIZ and entered the polar basin; and an undisturbed case. The MIZEX-84 period can be divided into three synoptic time periods. The first and the last were situations when the storms passed to the south and east of the Fram Striates. During the middle period the storms passed through the straits in response to the development of a closed upper-level low over the north coast of Greenland. Three of the four storms which moved into the straits were moving north-northwest and filled or slowed significantly in the MIZ. The fourth was moving parallel to the MIZ. This would seem to show that the MIZ does not dominate but may affect storm movement. Keywords: Arctic Marginal Ice Zone. (Theses) Text Arctic East Greenland Greenland Greenland Sea Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Greenland |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Meteorology Snow Ice and Permafrost *WEATHER *METEOROLOGICAL PHENOMENA *SEA ICE POLAR REGIONS COASTAL REGIONS INTENSITY THESES ICE STORMS NORTH(DIRECTION) LOW STRENGTH BASINS(GEOGRAPHIC) ARCTIC REGIONS GREENLAND SEA EAST(DIRECTION) GREENLAND STRAITS Marginal ice zone |
spellingShingle |
Meteorology Snow Ice and Permafrost *WEATHER *METEOROLOGICAL PHENOMENA *SEA ICE POLAR REGIONS COASTAL REGIONS INTENSITY THESES ICE STORMS NORTH(DIRECTION) LOW STRENGTH BASINS(GEOGRAPHIC) ARCTIC REGIONS GREENLAND SEA EAST(DIRECTION) GREENLAND STRAITS Marginal ice zone Phegley,Larry D Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
topic_facet |
Meteorology Snow Ice and Permafrost *WEATHER *METEOROLOGICAL PHENOMENA *SEA ICE POLAR REGIONS COASTAL REGIONS INTENSITY THESES ICE STORMS NORTH(DIRECTION) LOW STRENGTH BASINS(GEOGRAPHIC) ARCTIC REGIONS GREENLAND SEA EAST(DIRECTION) GREENLAND STRAITS Marginal ice zone |
description |
This thesis summarizes meteorological conditions occurring in the Marginal Ice Zone Experiment (MIZEX-84), conducted in the East Greenland Sea during the summer of 1984, are summarized. It includes a discussion of the synoptic and mesoscale conditions. The three cases discussed are: a weak storm which filled over the marginal ice zone (MIZ); an intense storm which transited the MIZ and entered the polar basin; and an undisturbed case. The MIZEX-84 period can be divided into three synoptic time periods. The first and the last were situations when the storms passed to the south and east of the Fram Striates. During the middle period the storms passed through the straits in response to the development of a closed upper-level low over the north coast of Greenland. Three of the four storms which moved into the straits were moving north-northwest and filled or slowed significantly in the MIZ. The fourth was moving parallel to the MIZ. This would seem to show that the MIZ does not dominate but may affect storm movement. Keywords: Arctic Marginal Ice Zone. (Theses) |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
Phegley,Larry D |
author_facet |
Phegley,Larry D |
author_sort |
Phegley,Larry D |
title |
Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
title_short |
Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
title_full |
Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
title_fullStr |
Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
title_full_unstemmed |
Synoptic/Mesoscale Meteorological Features in the Marginal Ice Zone. |
title_sort |
synoptic/mesoscale meteorological features in the marginal ice zone. |
publishDate |
1985 |
url |
http://www.dtic.mil/docs/citations/ADA165016 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA165016 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic East Greenland Greenland Greenland Sea Ice permafrost Sea ice |
genre_facet |
Arctic East Greenland Greenland Greenland Sea Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA165016 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766329922861662208 |