The diagnosis of a pre-blocking explosively-developing extratropical cyclone system

This paper presents the diagnosis of an extratropical cyclone that developed explosively from 18 to 19 January 1979 over the North Atlantic Ocean. The diagnosis applies data obtained from the Goddard Laboratory for Atmospheres FGGE SOP-1 level III-b global analyses on a 4° latitude by 5° longitude g...

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Main Authors: Smith, Phillip J., Lupo, Anthony R., 1966-, Uhl, Mary A.
Other Authors: University of Missouri-Columbia. College of Agriculture, Food and Natural Resources (CAFNR). School of Natural Resources. Department of Soil, Environmental and Atmospheric Sciences.
Format: Article in Journal/Newspaper
Language:English
Published: Munksgaard 1992
Subjects:
Online Access:http://hdl.handle.net/10355/2410
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author Smith, Phillip J.
Lupo, Anthony R., 1966-
Uhl, Mary A.
author2 University of Missouri-Columbia. College of Agriculture, Food and Natural Resources (CAFNR). School of Natural Resources. Department of Soil, Environmental and Atmospheric Sciences.
author_facet Smith, Phillip J.
Lupo, Anthony R., 1966-
Uhl, Mary A.
author_sort Smith, Phillip J.
collection University of Missouri: MOspace
description This paper presents the diagnosis of an extratropical cyclone that developed explosively from 18 to 19 January 1979 over the North Atlantic Ocean. The diagnosis applies data obtained from the Goddard Laboratory for Atmospheres FGGE SOP-1 level III-b global analyses on a 4° latitude by 5° longitude grid to the extended height tendency and the Zwack-Okossi development equations. The cyclone developed initially in response to cyclonic vorticity advection downstream from an upper air trough, warm air advection in a strongly baroclinic region, and latent heat release in the cyclone domain. As development continued, thermal advection and latent heat release increased their role in forcing height falls in the cyclone domain, while the influence of vorticity advection decreased. Finally, development ceased when anticyclonic vorticity advection below 700 mb and adiabatic cooling in the ascending air combined to neutralize the influence of warm air advection and latent heat release.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
id ftunimissourimos:oai:mospace.umsystem.edu:10355/2410
institution Open Polar
language English
op_collection_id ftunimissourimos
op_relation University of Missouri-Columbia. College of Agriculture, Food and Natural Resources. School of Natural Resources. Department of Soil, Environmental and Atmospheric Sciences
Soil, Environmental and Atmospheric Sciences publications (MU)
Monthly Weather Review Volume 44 Issue 3 , pp. 236-251
0280-6495
http://hdl.handle.net/10355/2410
op_source http://solberg.snr.missouri.edu/gcc/
publishDate 1992
publisher Munksgaard
record_format openpolar
spelling ftunimissourimos:oai:mospace.umsystem.edu:10355/2410 2025-01-16T23:39:16+00:00 The diagnosis of a pre-blocking explosively-developing extratropical cyclone system Smith, Phillip J. Lupo, Anthony R., 1966- Uhl, Mary A. University of Missouri-Columbia. College of Agriculture, Food and Natural Resources (CAFNR). School of Natural Resources. Department of Soil, Environmental and Atmospheric Sciences. 1992-05 http://hdl.handle.net/10355/2410 English eng eng Munksgaard University of Missouri-Columbia. College of Agriculture, Food and Natural Resources. School of Natural Resources. Department of Soil, Environmental and Atmospheric Sciences Soil, Environmental and Atmospheric Sciences publications (MU) Monthly Weather Review Volume 44 Issue 3 , pp. 236-251 0280-6495 http://hdl.handle.net/10355/2410 http://solberg.snr.missouri.edu/gcc/ extratropical cyclone Cyclone forecasting Blocking (Meteorology) Article 1992 ftunimissourimos 2024-09-17T04:29:19Z This paper presents the diagnosis of an extratropical cyclone that developed explosively from 18 to 19 January 1979 over the North Atlantic Ocean. The diagnosis applies data obtained from the Goddard Laboratory for Atmospheres FGGE SOP-1 level III-b global analyses on a 4° latitude by 5° longitude grid to the extended height tendency and the Zwack-Okossi development equations. The cyclone developed initially in response to cyclonic vorticity advection downstream from an upper air trough, warm air advection in a strongly baroclinic region, and latent heat release in the cyclone domain. As development continued, thermal advection and latent heat release increased their role in forcing height falls in the cyclone domain, while the influence of vorticity advection decreased. Finally, development ceased when anticyclonic vorticity advection below 700 mb and adiabatic cooling in the ascending air combined to neutralize the influence of warm air advection and latent heat release. Article in Journal/Newspaper North Atlantic University of Missouri: MOspace
spellingShingle extratropical cyclone
Cyclone forecasting
Blocking (Meteorology)
Smith, Phillip J.
Lupo, Anthony R., 1966-
Uhl, Mary A.
The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title_full The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title_fullStr The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title_full_unstemmed The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title_short The diagnosis of a pre-blocking explosively-developing extratropical cyclone system
title_sort diagnosis of a pre-blocking explosively-developing extratropical cyclone system
topic extratropical cyclone
Cyclone forecasting
Blocking (Meteorology)
topic_facet extratropical cyclone
Cyclone forecasting
Blocking (Meteorology)
url http://hdl.handle.net/10355/2410