FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE
Numerous cold fronts associated with mature extratropical storms sweep the coast of Chile every year. The large expanses of the Southern Pacific Ocean offer an ideal setting for up to 4000-km long cold fronts to develop as their parent cyclones travel from Australia to South America. These fronts so...
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Format: | Article |
Language: | English |
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Universidad de Concepción
2004-01-01
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Series: | Gayana |
Online Access: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028 |
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author | Jérôme Patoux Robert A. Brown |
author_facet | Jérôme Patoux Robert A. Brown |
author_sort | Jérôme Patoux |
collection | DOAJ |
description | Numerous cold fronts associated with mature extratropical storms sweep the coast of Chile every year. The large expanses of the Southern Pacific Ocean offer an ideal setting for up to 4000-km long cold fronts to develop as their parent cyclones travel from Australia to South America. These fronts sometimes break and spawn secondary cyclones that deepen significantly in one or two days. Examples of such frontal waves will be shown and discussed. An attribution technique applied to scatterometer wind measurements is used to diagnose the development of those frontal waves. Necessary conditions for their development are revealed |
first_indexed | 2024-12-20T22:51:49Z |
format | Article |
id | doaj.art-604e9ac2ad824918a292cd81d583af1c |
institution | Directory Open Access Journal |
issn | 0717-652X 0717-6538 |
language | English |
last_indexed | 2024-12-20T22:51:49Z |
publishDate | 2004-01-01 |
publisher | Universidad de Concepción |
record_format | Article |
series | Gayana |
spelling | doaj.art-604e9ac2ad824918a292cd81d583af1c2022-12-21T19:24:14ZengUniversidad de ConcepciónGayana0717-652X0717-65382004-01-01682474475FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONEJérôme PatouxRobert A. BrownNumerous cold fronts associated with mature extratropical storms sweep the coast of Chile every year. The large expanses of the Southern Pacific Ocean offer an ideal setting for up to 4000-km long cold fronts to develop as their parent cyclones travel from Australia to South America. These fronts sometimes break and spawn secondary cyclones that deepen significantly in one or two days. Examples of such frontal waves will be shown and discussed. An attribution technique applied to scatterometer wind measurements is used to diagnose the development of those frontal waves. Necessary conditions for their development are revealedhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028 |
spellingShingle | Jérôme Patoux Robert A. Brown FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE Gayana |
title | FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
title_full | FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
title_fullStr | FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
title_full_unstemmed | FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
title_short | FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
title_sort | fronts and frontal waves over the southern cone |
url | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028 |
work_keys_str_mv | AT jeromepatoux frontsandfrontalwavesoverthesoutherncone AT robertabrown frontsandfrontalwavesoverthesoutherncone |