The 2017 coastal El Niño

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dc.contributor.authorTakahashi, Ken
dc.contributor.authorAliaga-Nestares, V.
dc.contributor.authorAvalos, G.
dc.contributor.authorBouchon, M.
dc.contributor.authorCastro, A.
dc.contributor.authorCruzado, L.
dc.contributor.authorDewitte, Boris
dc.contributor.authorGutiérrez, D.
dc.contributor.authorLavado-Casimiro, W.
dc.contributor.authorMarengo, J.
dc.contributor.authorMartínez Grimaldo, Alejandra
dc.contributor.authorMosquera Vásquez, Kobi Alberto
dc.contributor.authorQuispe, N.
dc.date.accessioned2018-09-18T20:09:01Z
dc.date.available2018-09-18T20:09:01Z
dc.date.issued2018-08
dc.description.abstractThe original concept of El Niño consisted of anomalously high sea surface temperature and heavy rainfall along the arid northern coast of Peru (Carranza 1891; Carrillo 1893). The concept evolved into the El Niño–Southern Oscillation (ENSO; Bjerknes 1969), although the original El Niño and the Southern Oscillation do not necessarily have the same variability (Deser and Wallace 1987), and the strong El Niño episode in early 1925 coincided with cold-to-neutral ENSO conditions (Takahashi and Martínez 2017). To distinguish the near-coastal El Niño from the warm ENSO phase, Peru operationally defines the “coastal El Niño” based on the seasonal Niño 1+2 SST anomaly (ENFEN 2012; L’Heureux et al. 2017). While recent attention has been brought to the concept of ENSO diversity (e.g., “central Pacific” vs “eastern Pacific” events; Capotondi et al. 2015), the coastal El Niño represents another facet of ENSO that requires further study in terms of its mechanisms and predictability.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationTakahashi, K., Aliaga-Nestares, V., Avalos, G., Bouchon, M., Castro, A., Cruzado, L., … Quispe, N. (2018). The 2017 coastal El Niño [in “State of the Climate in 2017”].==$Bulletin of American Meteorological Society, 99$==(8), S210–S211.es_ES
dc.identifier.govdocindex-oti2018
dc.identifier.journalBulletin of the American Meteorological Societyes_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/2988
dc.language.isoenges_ES
dc.publisherAmerican Meteorological Societyes_ES
dc.relation.ispartofhttps://doi.org/10.1175/2018BAMSStateoftheClimate.1
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.uri(c) American Meteorological Societyes_ES
dc.subjectEl Niñoes_ES
dc.subjectAtmospheric precipitationes_ES
dc.subjectClimate changees_ES
dc.subjectMeteorologyes_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.00es_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.09es_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.10es_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.11es_ES
dc.titleThe 2017 coastal El Niñoes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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