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...

Full description

Bibliographic Details
Main Authors: Jérôme Patoux, Robert A. Brown
Format: Article
Language:English
Published: Universidad de Concepción 2004-01-01
Series:Gayana
Online Access:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028
_version_ 1819001602354184192
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