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Eastern Pacific coastal dynamics and the Intra-Americas summer low level jet

dc.creatorTrasviña Castro, Armando
dc.creatorAmador Astúa, Jorge Alberto
dc.date.accessioned2023-08-08T21:25:46Z
dc.date.available2023-08-08T21:25:46Z
dc.date.issued2005
dc.description.abstractIt is generally agreed that the circulation of the Eastern Pacific off México and Central America is forced in the summer by the large-scale circulation, namely the North Equatorial Countercurrent, and in the winter by strong offshore winds blowing through mountain passes in Mexico and Central America.es_ES
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI)es_ES
dc.identifier.citationhttps://meetings.copernicus.org/www.cosis.net/abstracts/EGU05/09826/EGU05-J-09826.pdfes_ES
dc.identifier.other1607-7962/gra/EGU05-A-09826
dc.identifier.urihttps://hdl.handle.net/10669/89825
dc.language.isoenges_ES
dc.rightsacceso abierto
dc.sourceGeophysical Research Abstracts, vol.7,(09826)es_ES
dc.subjectINTRA-AMERICAS SUMMERes_ES
dc.subjectEASTERN PACIFICes_ES
dc.titleEastern Pacific coastal dynamics and the Intra-Americas summer low level jetes_ES
dc.typecontribución de congresoes_ES

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