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http://hdl.handle.net/2445/124852
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DC Field | Value | Language |
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dc.contributor.author | King, Martin P. | - |
dc.contributor.author | Herceg-Bulic, Ivana | - |
dc.contributor.author | Bladé, Ileana | - |
dc.contributor.author | García-Serrano, Javier | - |
dc.contributor.author | Keenlyside, Noel | - |
dc.contributor.author | Kucharski, Fred | - |
dc.contributor.author | Li, Camille | - |
dc.contributor.author | Sobolowski, Stefan | - |
dc.date.accessioned | 2018-09-26T16:25:38Z | - |
dc.date.available | 2018-09-26T16:25:38Z | - |
dc.date.issued | 2018-07-23 | - |
dc.identifier.issn | 0003-0007 | - |
dc.identifier.uri | http://hdl.handle.net/2445/124852 | - |
dc.description.abstract | Recent studies have indicated the importance of fall climate forcings and teleconnections in influencing the climate of the northern mid-to-high latitudes. Here, we present some exploratory analyses using observational data and seasonal hindcasts, with the aim of highlighting the potential of the El Niño-Southern Oscillation (ENSO) as a driver of climate variability during boreal late fall/early winter (November/December) in the North Atlantic-European sector and motivating further research on this relatively unexplored topic. The atmospheric ENSO teleconnection in November/December is reminiscent of the East Atlantic pattern and distinct from the well-known arching extratropical Rossby wavetrain found from January to March. Temperature and precipitation over Europe in November are positively correlated with the Niño3.4 index, which suggests a potentially important ENSO climate impact during late fall. In particular, the ENSO-related temperature anomaly extends over a much larger area than during the subsequent winter month | - |
dc.format.extent | 7 p. | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | American Meteorological Society | - |
dc.relation.isformatof | Reproducció del document publicat a: https://doi.org/10.1175/BAMS-D-17-0020.1 | - |
dc.relation.ispartof | Bulletin of the American Meteorological Society, 2018, vol. 99, num. 7, p. 1337-1343 | - |
dc.relation.uri | https://doi.org/10.1175/BAMS-D-17-0020.1 | - |
dc.rights | (c) American Meteorological Society, 2018 | - |
dc.source | Articles publicats en revistes (Física Aplicada) | - |
dc.subject.classification | Canvi climàtic | - |
dc.subject.classification | Mediterrània (Regió) | - |
dc.subject.classification | Precipitacions (Meteorologia) | - |
dc.subject.classification | Corrent del Niño | - |
dc.subject.other | Climatic change | - |
dc.subject.other | Mediterranean Region | - |
dc.subject.other | Precipitations (Meteorology) | - |
dc.subject.other | El Niño Current | - |
dc.title | Importance of late fall ENSO teleconnection in the Euro-Atlantic sector | - |
dc.type | info:eu-repo/semantics/article | - |
dc.type | info:eu-repo/semantics/publishedVersion | - |
dc.identifier.idgrec | 676087 | - |
dc.date.updated | 2018-09-26T16:25:38Z | - |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | - |
Appears in Collections: | Articles publicats en revistes (Física Aplicada) |
Files in This Item:
File | Description | Size | Format | |
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676087.pdf | 3.99 MB | Adobe PDF | View/Open |
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