HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN

A general survey is made of the relation between the exchanges of heat and moisture at the ocean-atmosphere interface on the one side, and the development of extratropical cyclones on the other. The methods of computing eddy and other exchanges are described. With the aid of a system of coordinates...

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Main Authors: PETTERSSEN,SVERRE, BRADBURY,DOROTHY L., PEDERSEN,KAARE
Other Authors: WEATHER FORECASTING RESEARCH CENTER UNIV OF CHICAGO ILL
Format: Text
Language:English
Published: 1961
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0260975
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260975
id ftdtic:AD0260975
record_format openpolar
spelling ftdtic:AD0260975 2023-05-15T17:30:24+02:00 HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN PETTERSSEN,SVERRE BRADBURY,DOROTHY L. PEDERSEN,KAARE WEATHER FORECASTING RESEARCH CENTER UNIV OF CHICAGO ILL 1961-06 text/html http://www.dtic.mil/docs/citations/AD0260975 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260975 en eng http://www.dtic.mil/docs/citations/AD0260975 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *AIR MASS ANALYSIS *HEAT TRANSFER *WEATHER FORECASTING ATMOSPHERES ATMOSPHERE MODELS CYCLONES METEOROLOGICAL CHARTS METEOROLOGY MOISTURE PROBABILITY STATISTICAL ANALYSIS Text 1961 ftdtic 2016-02-21T12:05:49Z A general survey is made of the relation between the exchanges of heat and moisture at the ocean-atmosphere interface on the one side, and the development of extratropical cyclones on the other. The methods of computing eddy and other exchanges are described. With the aid of a system of coordinates in which grid point identify distance from the frontal zone and from the cyclone center, cyclone models are constructed as mean states each representing a large number of individual cases. The stages of cyclone development represented by the models are: the nascent cyclone wave, the warm-sector cyclone, the partly occluded cyclone, the fully occluded cyclone, and the cold-core frontless cyclone. The vorticity equation and the thermodynamic energy equation are used to obtain a diagnostic equation for the vertical velocity and a prognostic equation for the rate of change of the thickness of an isobaric layer, both containing the terms which represent the sensible heat and the release of latent heat. The equations were tested on 10 synoptic situations on the North Atlantic Ocean. (Author) Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic *AIR MASS ANALYSIS
*HEAT TRANSFER
*WEATHER FORECASTING
ATMOSPHERES
ATMOSPHERE MODELS
CYCLONES
METEOROLOGICAL CHARTS
METEOROLOGY
MOISTURE
PROBABILITY
STATISTICAL ANALYSIS
spellingShingle *AIR MASS ANALYSIS
*HEAT TRANSFER
*WEATHER FORECASTING
ATMOSPHERES
ATMOSPHERE MODELS
CYCLONES
METEOROLOGICAL CHARTS
METEOROLOGY
MOISTURE
PROBABILITY
STATISTICAL ANALYSIS
PETTERSSEN,SVERRE
BRADBURY,DOROTHY L.
PEDERSEN,KAARE
HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
topic_facet *AIR MASS ANALYSIS
*HEAT TRANSFER
*WEATHER FORECASTING
ATMOSPHERES
ATMOSPHERE MODELS
CYCLONES
METEOROLOGICAL CHARTS
METEOROLOGY
MOISTURE
PROBABILITY
STATISTICAL ANALYSIS
description A general survey is made of the relation between the exchanges of heat and moisture at the ocean-atmosphere interface on the one side, and the development of extratropical cyclones on the other. The methods of computing eddy and other exchanges are described. With the aid of a system of coordinates in which grid point identify distance from the frontal zone and from the cyclone center, cyclone models are constructed as mean states each representing a large number of individual cases. The stages of cyclone development represented by the models are: the nascent cyclone wave, the warm-sector cyclone, the partly occluded cyclone, the fully occluded cyclone, and the cold-core frontless cyclone. The vorticity equation and the thermodynamic energy equation are used to obtain a diagnostic equation for the vertical velocity and a prognostic equation for the rate of change of the thickness of an isobaric layer, both containing the terms which represent the sensible heat and the release of latent heat. The equations were tested on 10 synoptic situations on the North Atlantic Ocean. (Author)
author2 WEATHER FORECASTING RESEARCH CENTER UNIV OF CHICAGO ILL
format Text
author PETTERSSEN,SVERRE
BRADBURY,DOROTHY L.
PEDERSEN,KAARE
author_facet PETTERSSEN,SVERRE
BRADBURY,DOROTHY L.
PEDERSEN,KAARE
author_sort PETTERSSEN,SVERRE
title HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
title_short HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
title_full HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
title_fullStr HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
title_full_unstemmed HEAT EXCHANGE AND CYCLONE DEVELOPMENT ON THE NORTH ATLANTIC OCEAN
title_sort heat exchange and cyclone development on the north atlantic ocean
publishDate 1961
url http://www.dtic.mil/docs/citations/AD0260975
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260975
genre North Atlantic
genre_facet North Atlantic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0260975
op_rights APPROVED FOR PUBLIC RELEASE
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