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The complex behavior of El Niño winter 2015-2016

dc.contributor.authorPalmeiro Núñez, Froila María
dc.contributor.authorIza San Juan, Maddalen
dc.contributor.authorBarriopedro Cepero, David
dc.contributor.authorCalvo Fernández, Natalia
dc.contributor.authorGarcía Herrera, Ricardo Francisco
dc.date.accessioned2023-06-17T21:58:00Z
dc.date.available2023-06-17T21:58:00Z
dc.date.issued2017-03-28
dc.description©2017. American Geophysical Union. All Rights Reserved. We acknowledge the ECMWF for providing ERA-40 and ERA-Interim reanalysis data (http://apps.ecmwf.int/datasets/), the Global Precipitation Climatology Centre for the precipitation data (ftp://ftp-anon.dwd.de/pub/data/gpcc/html/download_gate.html), and the Met Office Hadley Centre for the HadISST1 data (http://www.metoffice.gov.uk/hadobs/hadisst/data/download.html). We thank Kate Willett and an anonymous reviewer for their helpful comments. This work was supported by the Spanish Ministry of Economy and Competitiveness through the PALEOSTRAT (CGL2015-69699-R) project and the European Project 603557-STRATOCLIM under program FP7-ENV.2013.6.1-2. F.M. Palmeiro was funded by grant BES-2013-063906.
dc.description.abstractThis paper examines the outstanding characteristics of the strong 2015-2016 El Nino (EN) winter and its impact over the European region through the stratosphere. Despite being classified as a strong eastern Pacific (EP) EN event, our analysis reveals an anomalous behavior, with some signatures that are more typical of central Pacific (CP) EN events instead. They include (i) a record-breaking value of the CP index, (ii) a stronger polar vortex in early and midwinter, due to reduced upward wave activity and a weakened Aleutian low, and (iii) the occurrence of one of the earliest stratospheric final warmings (SFWs) on record, which are more prone to occur during CP-EN. Following the SFW, a stratospheric influence on the Euro-Atlantic sector is reported in spring, with persistent Greenland blocking resulting in extreme precipitation over some southern European regions. Results highlight the importance of considering early SFWs as mediators of El Nino teleconnections.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipUnión Europea. FP7
dc.description.sponsorshipMinisterio de Economía y Competitividad (MINECO)
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/43116
dc.identifier.doi10.1002/2017GL072920
dc.identifier.issn0094-8276
dc.identifier.officialurlhttp://dx.doi.org/10.1002/2017GL072920
dc.identifier.relatedurlhttp://onlinelibrary.wiley.com/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/17857
dc.issue.number6
dc.journal.titleGeophysical research letters
dc.language.isoeng
dc.page.final2910
dc.page.initial2902
dc.publisherAmerican Geophysical Union
dc.relation.projectIDSTRATOCLIM (603557)
dc.relation.projectIDPALEOSTRAT (CGL2015-69699-R)
dc.relation.projectIDBES-2013-063906
dc.rights.accessRightsopen access
dc.subject.cdu52
dc.subject.keywordStratospheric sudden warmings
dc.subject.keywordNorth-Atlantic
dc.subject.keywordEnso
dc.subject.keywordVariability
dc.subject.keywordOscillation
dc.subject.keywordReanalysis
dc.subject.keywordBlocking
dc.subject.keywordImpact
dc.subject.keywordOnset
dc.subject.keywordModel
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.titleThe complex behavior of El Niño winter 2015-2016
dc.typejournal article
dc.volume.number44
dspace.entity.typePublication
relation.isAuthorOfPublication79629e81-2e7b-476b-be93-3773246986a3
relation.isAuthorOfPublication71d8f23d-ceaf-4f5f-8434-10a193bc3835
relation.isAuthorOfPublication3cfa985b-0ebd-44fb-b791-312638313455
relation.isAuthorOfPublication194b877d-c391-483e-9b29-31a99dff0a29
relation.isAuthorOfPublication.latestForDiscovery71d8f23d-ceaf-4f5f-8434-10a193bc3835

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