A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system
A synoptic investigation employing quasi-Lagrangian diagnostic techniques was conducted for a North Atlantic Ocean polar flow undergoing a period or rapid cyclogenesis. The polar flow was of relatively small horizontal scale and developed in a region of low static stability and large low-level baroc...
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Other Authors: | , , , |
Format: | Thesis |
Language: | English |
Published: |
Monterey, California. Naval Postgraduate School
1983
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Online Access: | https://hdl.handle.net/10945/19963 |
_version_ | 1832475521999437824 |
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author | Cook, William A. |
author2 | Wash, Carlyle H. Naval Postgraduate School (U.S.) Meteorology Elsberry, Russell L. |
author_facet | Cook, William A. |
author_sort | Cook, William A. |
collection | Naval Postgraduate School: Calhoun |
description | A synoptic investigation employing quasi-Lagrangian diagnostic techniques was conducted for a North Atlantic Ocean polar flow undergoing a period or rapid cyclogenesis. The polar flow was of relatively small horizontal scale and developed in a region of low static stability and large low-level baroclinity, which is consistent with theoretical studies. Rapid surface pressure falls and vigorous circulation increases correlate well with the observed maxima in low-level inward mass transport and upper-level mass outflow, and are temporarily coincident with the incursion of to forward divergence quadrant of a jet streak into the budget volume. The most rapid increases of absolute vorticity occurred in the 250 to 300 mb layer, and are related to combined contributions of positive vorticity advection and vertical redistribution processes. The dominant forcing of low-level absolute vorticity increases comes primarily from the divergence source term. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/aquasilagrangidi1094519963 |
format | Thesis |
genre | North Atlantic |
genre_facet | North Atlantic |
id | ftnavalpschool:oai:calhoun.nps.edu:10945/19963 |
institution | Open Polar |
language | English |
op_collection_id | ftnavalpschool |
op_relation | https://hdl.handle.net/10945/19963 |
op_rights | This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. |
publishDate | 1983 |
publisher | Monterey, California. Naval Postgraduate School |
record_format | openpolar |
spelling | ftnavalpschool:oai:calhoun.nps.edu:10945/19963 2025-05-18T14:04:46+00:00 A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system Cook, William A. Wash, Carlyle H. Naval Postgraduate School (U.S.) Meteorology Elsberry, Russell L. 1983-09 application/pdf https://hdl.handle.net/10945/19963 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/19963 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. North Atlantic Quasi-Langrangian diagnostics Mass budget Stability analysis Vorticity budget Explosive maritime cyclogenesis Polar low Meteorology Maritime Thesis 1983 ftnavalpschool 2025-04-29T04:29:37Z A synoptic investigation employing quasi-Lagrangian diagnostic techniques was conducted for a North Atlantic Ocean polar flow undergoing a period or rapid cyclogenesis. The polar flow was of relatively small horizontal scale and developed in a region of low static stability and large low-level baroclinity, which is consistent with theoretical studies. Rapid surface pressure falls and vigorous circulation increases correlate well with the observed maxima in low-level inward mass transport and upper-level mass outflow, and are temporarily coincident with the incursion of to forward divergence quadrant of a jet streak into the budget volume. The most rapid increases of absolute vorticity occurred in the 250 to 300 mb layer, and are related to combined contributions of positive vorticity advection and vertical redistribution processes. The dominant forcing of low-level absolute vorticity increases comes primarily from the divergence source term. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/aquasilagrangidi1094519963 Thesis North Atlantic Naval Postgraduate School: Calhoun |
spellingShingle | North Atlantic Quasi-Langrangian diagnostics Mass budget Stability analysis Vorticity budget Explosive maritime cyclogenesis Polar low Meteorology Maritime Cook, William A. A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title | A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title_full | A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title_fullStr | A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title_full_unstemmed | A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title_short | A quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
title_sort | quasi-lagrangian diagnostics investigation of rapid cyclogenesis in a polar air system |
topic | North Atlantic Quasi-Langrangian diagnostics Mass budget Stability analysis Vorticity budget Explosive maritime cyclogenesis Polar low Meteorology Maritime |
topic_facet | North Atlantic Quasi-Langrangian diagnostics Mass budget Stability analysis Vorticity budget Explosive maritime cyclogenesis Polar low Meteorology Maritime |
url | https://hdl.handle.net/10945/19963 |