The 2017 coastal El Niño

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.
dc.description.peer-reviewPor pares
dc.formatapplication/pdf
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.
dc.identifier.govdocindex-oti2018
dc.identifier.journalBulletin of the American Meteorological Society
dc.identifier.urihttp://hdl.handle.net/20.500.12816/2988
dc.language.isoeng
dc.publisherAmerican Meteorological Society
dc.relation.ispartofhttps://doi.org/10.1175/2018BAMSStateoftheClimate.1
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rights.uri(c) American Meteorological Society
dc.subjectEl Niño
dc.subjectAtmospheric precipitation
dc.subjectClimate change
dc.subjectMeteorology
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.00
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.09
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.10
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.11
dc.titleThe 2017 coastal El Niño
dc.typeinfo:eu-repo/semantics/article

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