A three‐front model for synoptic analyses

Abstract A model for synoptic frontal analyses derived from frontal‐contour‐chart studies is described. Three frontal systems named the polar front, the maritime arctic front and the continental arctic front are necessary to portray adequately the thermal‐frontal structure of the atmosphere. In‐phas...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Author: Penner, C. M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1955
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.49708134710
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49708134710
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49708134710
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spelling crwiley:10.1002/qj.49708134710 2024-06-02T08:01:03+00:00 A three‐front model for synoptic analyses Penner, C. M. 1955 http://dx.doi.org/10.1002/qj.49708134710 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49708134710 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49708134710 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 81, issue 347, page 89-91 ISSN 0035-9009 1477-870X journal-article 1955 crwiley https://doi.org/10.1002/qj.49708134710 2024-05-06T07:01:25Z Abstract A model for synoptic frontal analyses derived from frontal‐contour‐chart studies is described. Three frontal systems named the polar front, the maritime arctic front and the continental arctic front are necessary to portray adequately the thermal‐frontal structure of the atmosphere. In‐phase wave development on at least two of the frontal systems occurs during major cylogenesis. The three‐front (or four‐air‐mass) cyclone is verified by aerological analyses while the classical occlusion model is not usually observed. Article in Journal/Newspaper Arctic Wiley Online Library Arctic Quarterly Journal of the Royal Meteorological Society 81 347 89 91
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract A model for synoptic frontal analyses derived from frontal‐contour‐chart studies is described. Three frontal systems named the polar front, the maritime arctic front and the continental arctic front are necessary to portray adequately the thermal‐frontal structure of the atmosphere. In‐phase wave development on at least two of the frontal systems occurs during major cylogenesis. The three‐front (or four‐air‐mass) cyclone is verified by aerological analyses while the classical occlusion model is not usually observed.
format Article in Journal/Newspaper
author Penner, C. M.
spellingShingle Penner, C. M.
A three‐front model for synoptic analyses
author_facet Penner, C. M.
author_sort Penner, C. M.
title A three‐front model for synoptic analyses
title_short A three‐front model for synoptic analyses
title_full A three‐front model for synoptic analyses
title_fullStr A three‐front model for synoptic analyses
title_full_unstemmed A three‐front model for synoptic analyses
title_sort three‐front model for synoptic analyses
publisher Wiley
publishDate 1955
url http://dx.doi.org/10.1002/qj.49708134710
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49708134710
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49708134710
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Quarterly Journal of the Royal Meteorological Society
volume 81, issue 347, page 89-91
ISSN 0035-9009 1477-870X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/qj.49708134710
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 81
container_issue 347
container_start_page 89
op_container_end_page 91
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