Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity

Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity

 A study of the oceanic surface layer is presented, taking into account its vertical thermal structure and time-space variability. Oceanographic data from 37 cruises were used. The thickness of the isothermal layer and depth of the 26ºC isotherm were determined. The possible connection betw...

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Autores principales: Mitrani-Arenal, I, Díaz-Rodríguez, OO
Formato: Online
Lenguaje:eng
Publicado: Iniversidad Autónoma de Baja California 2004
Acceso en línea:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/182
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spelling oai:cienciasmarinas.com.mx:article-1822019-04-11T23:44:22Z Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity Relación entre la estructura térmica vertical de las aguas cubanas y la actividad de los ciclones tropicales Mitrani-Arenal, I Díaz-Rodríguez, OO thermal structure tropical cyclones Cuban waters capa isotérmica ciclones tropicales aguas cubanas  A study of the oceanic surface layer is presented, taking into account its vertical thermal structure and time-space variability. Oceanographic data from 37 cruises were used. The thickness of the isothermal layer and depth of the 26ºC isotherm were determined. The possible connection between the thermal characteristics of the sea surface layer and tropical cyclone activity was analyzed. The presence of ENSO was considered. We show that the thermal characteristics of Cuban waters are always favorable for tropical cyclone development. Se presenta un estudio de la estructura térmica vertical y la variabilidad espaciotemporal de la capa superficial oceánica en aguas cubanas, utilizando datos de 37 expediciones oceanográficas realizadas de 1966 a 1993. Se determinaron el espesor de la capa isotérmica y la profundidad de la isoterma de 26ºC. Se analizó el posible enlace entre las características térmicas de la capa superficial oceánica y el comportamiento de los ciclones tropicales. Se tuvo en cuenta la presencia de la Oscilación del Sur El Niño (ENOS). Se concluye que las características térmicas de las aguas cubanas siempre son favorables al desarrollo de los ciclones tropicales, independientemente de la presencia de ENOS. Iniversidad Autónoma de Baja California 2004-03-06 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo Arbitrado application/pdf https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/182 10.7773/cm.v30i2.182 Ciencias Marinas; Vol. 30 No. 2 (2004); 335-341 Ciencias Marinas; Vol. 30 Núm. 2 (2004); 335-341 2395-9053 0185-3880 eng https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/182/157
institution Ciencias Marinas
collection OJS
language eng
format Online
author Mitrani-Arenal, I
Díaz-Rodríguez, OO
spellingShingle Mitrani-Arenal, I
Díaz-Rodríguez, OO
Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
author_facet Mitrani-Arenal, I
Díaz-Rodríguez, OO
author_sort Mitrani-Arenal, I
title Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
title_short Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
title_full Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
title_fullStr Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
title_full_unstemmed Relationship between the thermal vertical structure of Cuban waters and tropical cyclone activity
title_sort relationship between the thermal vertical structure of cuban waters and tropical cyclone activity
description  A study of the oceanic surface layer is presented, taking into account its vertical thermal structure and time-space variability. Oceanographic data from 37 cruises were used. The thickness of the isothermal layer and depth of the 26ºC isotherm were determined. The possible connection between the thermal characteristics of the sea surface layer and tropical cyclone activity was analyzed. The presence of ENSO was considered. We show that the thermal characteristics of Cuban waters are always favorable for tropical cyclone development.
publisher Iniversidad Autónoma de Baja California
publishDate 2004
url https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/182
_version_ 1715723940047880192

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