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...
Guardado en:
| Autores principales: | , |
|---|---|
| Lenguaje: | English |
| Publicado: |
Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción
2004
|
| Acceso en línea: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028 |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| id |
oai:scielo:S0717-65382004000300028 |
|---|---|
| record_format |
dspace |
| spelling |
oai:scielo:S0717-653820040003000282005-05-16FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONEPatoux,JérômeBrown,Robert A.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 revealedinfo:eu-repo/semantics/openAccessFacultad de Ciencias Naturales y Oceanográficas, Universidad de ConcepciónGayana (Concepción) v.68 n.2 suppl.TIIProc 20042004-01-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028en10.4067/S0717-65382004000300028 |
| institution |
Scielo Chile |
| collection |
Scielo Chile |
| language |
English |
| 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 |
| author |
Patoux,Jérôme Brown,Robert A. |
| spellingShingle |
Patoux,Jérôme Brown,Robert A. FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
| author_facet |
Patoux,Jérôme Brown,Robert A. |
| author_sort |
Patoux,Jérôme |
| title |
FRONTS AND FRONTAL WAVES OVER THE SOUTHERN CONE |
| title_short |
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_sort |
fronts and frontal waves over the southern cone |
| publisher |
Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción |
| publishDate |
2004 |
| url |
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382004000300028 |
| work_keys_str_mv |
AT patouxjerome frontsandfrontalwavesoverthesoutherncone AT brownroberta frontsandfrontalwavesoverthesoutherncone |
| _version_ |
1718442078980014080 |