Ekman transport patterns in the area close to the Galician coast (NW, Spain)

A 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekma...

ver descrição completa

Detalhes bibliográficos
Autores: Cabanas-López, José Manuel, Álvarez, I.
Formato: artículo
Fecha de publicación:2006
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/324166
Acesso em linha:http://hdl.handle.net/10261/324166
Access Level:acceso abierto
Palavra-chave:Centro Oceanográfico de Vigo
Medio Marino
id ES_50310ff738fddbed12944f8d6450be5e
oai_identifier_str oai:digital.csic.es:10261/324166
network_acronym_str ES
network_name_str España
repository_id_str
spelling Ekman transport patterns in the area close to the Galician coast (NW, Spain)Cabanas-López, José ManuelÁlvarez, I.Centro Oceanográfico de VigoMedio MarinoA 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekman transport showed different seasonal patterns. Thus, the summer pattern is characterized by transport pointing seaward (upwelling favourable) practically perpendicular to the shoreline, while the winter pattern is characterized by transport pointing landward (downwelling favourable). Although the most favourable upwelling conditions were observed during summer, for the last 15 years the frequency of observed winter upwelling events is higher due to the prevalence of northerly winds.Sí202320232006info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/324166reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésCentro Oceanográfico de Vigoinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3241662026-05-22T06:33:51Z
dc.title.none.fl_str_mv Ekman transport patterns in the area close to the Galician coast (NW, Spain)
title Ekman transport patterns in the area close to the Galician coast (NW, Spain)
spellingShingle Ekman transport patterns in the area close to the Galician coast (NW, Spain)
Cabanas-López, José Manuel
Centro Oceanográfico de Vigo
Medio Marino
title_short Ekman transport patterns in the area close to the Galician coast (NW, Spain)
title_full Ekman transport patterns in the area close to the Galician coast (NW, Spain)
title_fullStr Ekman transport patterns in the area close to the Galician coast (NW, Spain)
title_full_unstemmed Ekman transport patterns in the area close to the Galician coast (NW, Spain)
title_sort Ekman transport patterns in the area close to the Galician coast (NW, Spain)
dc.creator.none.fl_str_mv Cabanas-López, José Manuel
Álvarez, I.
author Cabanas-López, José Manuel
author_facet Cabanas-López, José Manuel
Álvarez, I.
author_role author
author2 Álvarez, I.
author2_role author
dc.subject.none.fl_str_mv Centro Oceanográfico de Vigo
Medio Marino
topic Centro Oceanográfico de Vigo
Medio Marino
description A 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekman transport showed different seasonal patterns. Thus, the summer pattern is characterized by transport pointing seaward (upwelling favourable) practically perpendicular to the shoreline, while the winter pattern is characterized by transport pointing landward (downwelling favourable). Although the most favourable upwelling conditions were observed during summer, for the last 15 years the frequency of observed winter upwelling events is higher due to the prevalence of northerly winds.
publishDate 2006
dc.date.none.fl_str_mv 2006
2023
2023
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/324166
url http://hdl.handle.net/10261/324166
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Centro Oceanográfico de Vigo
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869407866643808256
score 15,811543