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dc.contributor.author Mosquera Vásquez, Kobi Alberto
dc.contributor.author Dewitte, Boris
dc.contributor.author Illig, Serena
dc.contributor.author Takahashi, Ken
dc.contributor.author Garric, G.
dc.date.accessioned 2018-09-17T17:04:32Z
dc.date.available 2018-09-17T17:04:32Z
dc.date.issued 2013-01
dc.identifier.govdoc index-oti2018 (NB)
dc.identifier.issn 21562202
dc.identifier.uri http://repositorio.igp.gob.pe/handle/IGP/2973
dc.description En: Journal of Geophysical Research: Oceans, v. 118, n. 1 (January 2013), p. 346-357.
dc.description.abstract "enomenon, with in particular an increased occurrence of so‐called Modoki or Central Pacific El Niños. Here the 2002/2003 El Niño, characterized as a Central Pacific El Niño, is studied from an Ocean General Circulation Model simulation. The focus is on the sequence of equatorial waves and their impact on zonal and vertical advection. The wave amplitude according to the most energetic baroclinic modes are first estimated, which allows inferring the sequence of the intraseasonal equatorial Kelvin (IKW) and Rossby (IRW) waves. It is shown that energetic downwelling IKWs, forced in the western‐central Pacific, crossed the equatorial Pacific. Reflections of IKWs into IRWs onto the zonally varying thermocline and eastern boundary are also observed. A simplified heat budget of the surface layer is then carried out to infer the dominant processes at work during the evolution of this event focusing on the wave‐induced advection terms. The results indicate that the warming phase (April–November 2002) is mainly controlled by zonal advection of mean temperature (accounted for by IKWs and locally wind‐driven current) and by vertical advection in the eastern Pacific. The cooling phase (December 2002 to April 2003) is dominated by a reduction in solar radiation and the IRW‐induced zonal advection of mean temperature respectively in the central and eastern equatorial Pacific. The recharge‐discharge process is also showed to be at work with the recharge (discharge) process operating mainly through the second (first) baroclinic mode." es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher Instituto Geofísico del Perú es_ES
dc.relation.uri https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2012JC008551 es_ES
dc.rights info:eu-repo/semantics/openAccess es_ES
dc.rights.uri http://creativecommons.org/licences/by-nc-nd/2.5/pe/ es_ES
dc.source Repositorio institucional - IGP es_ES
dc.subject Corriente El Niño es_ES
dc.subject Interacción océano-atmósfera es_ES
dc.subject Oceanografía--Costa del Pacífico (Perú) es_ES
dc.subject Cambio climático es_ES
dc.subject Temperatura del océano es_ES
dc.title The 2002/2003 El Niño: Equatorial waves sequence and their impact on sea surface temperature es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde Climatología es_ES
dc.subject.ocde Oceanografía es_ES
dc.subject.ocde Temperatura es_ES
dc.subject.ocde Efectos en el medio ambiente es_ES
dc.subject.ocde Medición es_ES
dc.identifier.journal Journal of Geophysical Research: Oceans es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi 10.1029/2012JC008551 es_ES

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