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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1955
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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 |
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Open Polar |
collection |
Wiley Online Library |
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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 |
_version_ |
1800745289668100096 |