A plausible atmospheric trigger for the 2017 coastal El Niño
Author
dc.contributor.author
Garreaud Salazar, René
Admission date
dc.date.accessioned
2018-10-08T16:14:40Z
Available date
dc.date.available
2018-10-08T16:14:40Z
Publication date
dc.date.issued
2018-04
Cita de ítem
dc.identifier.citation
Int. J. Climatol. 38 (Suppl.1): e1296–e1302 (2018)
es_ES
Identifier
dc.identifier.other
10.1002/joc.5426
Identifier
dc.identifier.uri
https://repositorio.uchile.cl/handle/2250/152026
Abstract
dc.description.abstract
The far eastern tropical Pacific experienced a rapid, marked warming in early 2017, causing torrential rains along the west coast of South America with a significant societal toll in Peru and Ecuador. This strong coastal El Nino was largely unpredicted, even a few weeks before its onset, and it developed differently from either central or eastern events. Here we provide an overview of the event, its impacts and concomitant atmospheric circulation. It is proposed that a remotely forced, sustained weakening of the free tropospheric westerly flow impinging the subtropical Andes leads to a relaxation of the southeasterly (SE) trades off the coast, which in turn may have warmed the eastern Pacific throughout the weakening of upwelling in a near-coastal band and the lessening of the evaporative cooling farther offshore.