Por favor, use este identificador para citar o enlazar a este item: http://hdl.handle.net/10261/126221
COMPARTIR / EXPORTAR:
logo share SHARE logo core CORE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invitar a revisión por pares abierta
Campo DC Valor Lengua/Idioma
dc.contributor.authorLosada, Teresaes_ES
dc.contributor.authorRodríguez-Fonseca, Belénes_ES
dc.date.accessioned2015-12-01T06:59:23Z-
dc.date.available2015-12-01T06:59:23Z-
dc.date.issued2015-11-17-
dc.identifier.citationClimate Dynamics, 47 (3-4): 1211-1224(2016)es_ES
dc.identifier.issn0930-7575-
dc.identifier.urihttp://hdl.handle.net/10261/126221-
dc.description.abstractIt has been shown that the atmospheric response to the Atlantic Equatorial Mode is non-stationary. After the 1970s, Sea Surface Temperature (SST) anomalies in the tropical Atlantic are able to alter the atmosphere in the tropical Pacific via modifications of the Walker circulation. Such changes could be related to the differences in the background state of the global SSTs before and after the 1970s, but also to changes in the interannual Equatorial Mode itself. In this work we first describe the differences in the interannual Equatorial Mode before and after the 1970s. Then we use two AGCMs to perform different sensitivity experiments changing the spatial structure of the Equatorial Mode, and we explore the differences in the atmospheric response over the tropical Pacific region to each of the SST patterns considered. It is shown that the changes in the Walker Atlantic–Pacific cell produced by the EM are stronger after the 1970s, and are reinforced by the change in the impact of the EM over the Indian Ocean and the Maritime Continent. It is also shown that, although the Atlantic–Pacific connection is established by the aforementioned changes in the Walker circulation between the two basins, the modulation of the Indian sector is crucial for a realistic simulation of such connection by climate models.es_ES
dc.description.sponsorshipThe research leading to these results has received funding from the European Union Seventh Framework Programme (FP7/2007–2013) under Grant Agreement No. 603521 (PREFACE Project), and by the Spanish Project CGL2012-38923-C02-01.es_ES
dc.language.isoenges_ES
dc.publisherSpringer Naturees_ES
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/603521es_ES
dc.relation.isversionofPreprintes_ES
dc.rightsopenAccesses_ES
dc.subjectTropical Atlantices_ES
dc.subjectClimate variabilityes_ES
dc.subjectEquatorial modees_ES
dc.subjectTropical teleconnectionses_ES
dc.titleTropical atmospheric response to decadal changes in the Atlantic Equatorial Modees_ES
dc.typeartículoes_ES
dc.identifier.doi10.1007/s00382-015-2897-2-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1007/s00382-015-2897-2es_ES
dc.identifier.e-issn1432-0894-
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.relation.csices_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
Aparece en las colecciones: (IGEO) Artículos
Ficheros en este ítem:
Fichero Descripción Tamaño Formato
CD_2016_Losada_RodriguezFonseca_ClimDyn_2015_PrePrint.pdf3,35 MBAdobe PDFVista previa
Visualizar/Abrir
Show simple item record

CORE Recommender

SCOPUSTM   
Citations

23
checked on 23-mar-2024

WEB OF SCIENCETM
Citations

22
checked on 22-feb-2024

Page view(s)

323
checked on 27-mar-2024

Download(s)

369
checked on 27-mar-2024

Google ScholarTM

Check

Altmetric

Altmetric


NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.