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Role of Stratospheric Sudden Warmings on the response to Central Pacific El Niño

dc.contributor.authorIza San Juan, Maddalen
dc.contributor.authorCalvo Fernández, Natalia
dc.date.accessioned2023-06-18T06:45:19Z
dc.date.available2023-06-18T06:45:19Z
dc.date.issued2015-04-16
dc.description© 2015. The Authors. We acknowledge the ECMWF for providing ERA-40 and ERA-Interim reanalysis data (http://apps.ecmwf.int/datasets/) and the NCEP/CPC for the Niño3 and Niño4 indices (http://www.cpc.ncep.noaa.gov/data/indices/). This work was supported by the Spanish Ministry of Economy and Competitiveness through the MATRES (CGL2012-34221) project and the European Project 603557-STRATOCLIM under program FP7-ENV.2013.6.1-2. The authors are grateful to R. R. García for his comments on the manuscript and to R. García Herrera and D. Barriopedro for their fruitful discussions. The constructive comments of two anonymous reviewers are gratefully acknowledged.
dc.description.abstractThe Northern Hemisphere (NH) polar stratospheric response to Central Pacific El Niño (CP-El Niño) events remains unclear. Contradictory results have been reported depending on the definition and events considered. We show that this is due to the prominent role of Stratospheric Sudden Warmings (SSWs), whose signal dominates the NH winter polar stratospheric response to CP-El Niño. In fact, the CP-El Niño signal is robust when the events are classified according to the occurrence of SSWs and displays opposite response in winters with and without SSWs. In the absence of SSWs, polar stratospheric responses to Central Pacific and Eastern Pacific El Niño are clearly distinguishable in early winter, in relation to differences in the Pacific-North American pattern. Our results demonstrate that the occurrence of SSWs needs to be taken into account when studying the stratospheric response to CP-El Niño and explain why different responses to CP-El Niño have been reported previously.
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), España
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/30790
dc.identifier.doi10.1002/2014GL062935
dc.identifier.issn0094-8276
dc.identifier.officialurlhttp://dx.doi.org/10.1002/2014GL062935
dc.identifier.relatedurlhttp://onlinelibrary.wiley.com/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/24039
dc.issue.number7
dc.journal.titleGeophysical research letters
dc.language.isoeng
dc.page.final2489
dc.page.initial2482
dc.publisherAmerican Geophysical Union
dc.relation.projectIDSTRATOCLIM (603557)
dc.relation.projectIDMATRES CGL2012-34221
dc.rightsAtribución 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/es/
dc.subject.cdu52
dc.subject.keywordEastern-Pacific
dc.subject.keywordNorth-Atlantic
dc.subject.keywordClimate
dc.subject.keywordEnso
dc.subject.keywordReanalysis
dc.subject.keywordEvents
dc.subject.keywordRegion
dc.subject.keywordModoki
dc.subject.keywordRim
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.titleRole of Stratospheric Sudden Warmings on the response to Central Pacific El Niño
dc.typejournal article
dc.volume.number42
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relation.isAuthorOfPublication.latestForDiscovery3cfa985b-0ebd-44fb-b791-312638313455

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