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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Main Author: Cook, William A.
Other Authors: Wash, Carlyle H., Naval Postgraduate School (U.S.), Meteorology, Elsberry, Russell L.
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1983
Subjects:
Online Access:https://hdl.handle.net/10945/19963
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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