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dc.contributor.authorChiodo, G.es_ES
dc.contributor.authorGarcía Herrera, Ricardoes_ES
dc.contributor.authorCalvo, N.es_ES
dc.contributor.authorVaquero, José Manueles_ES
dc.contributor.authorAñel, Juan A.es_ES
dc.contributor.authorBarriopedro, Davides_ES
dc.contributor.authorMatthes, K.es_ES
dc.date.accessioned2016-04-22T05:17:18Z-
dc.date.available2016-04-22T05:17:18Z-
dc.date.issued2016-03-07-
dc.identifier.citationEnvironmental Research Letters, 11 (3): 034015 (2016)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/131341-
dc.description.abstractSolar variability represents a source of uncertainty in the future forcings used in climate model simulations. Current knowledge indicates that a descent of solar activity into an extended minimum state is a possible scenario. With aid of experiments from a state-of-the-art Earth system model,we investigate the impact of a future solar minimum on Northern Hemisphere climate change projections. This scenario is constructed from recent 11 year solar-cycle minima of the solar spectral irradiance, and is therefore more conservative than the 'grand' minima employed in some previous modeling studies. Despite the small reduction in total solar irradiance (0.36 W m−2), relatively large responses emerge in the winter Northern Hemisphere, with a reduction in regional-scale projected warming by up to 40%. To identify the origin of the enhanced regional signals, we assess the role of the different mechanisms by performing additional experiments forced only by irradiance changes at different wavelengths of the solar spectrum. We find that a reduction in visible irradiance drives changes in the stationary wave pattern of the North Pacific and sea–ice cover. A decrease in UV irradiance leads to smaller surface signals, although its regional effects are not negligible. These results point to a distinct but additive role of UV and visible irradiance in the Earth's climate, and stress the need to account for solar forcing as a source of uncertainty in regional scale projections.es_ES
dc.description.sponsorshipThis work was supported by the Spanish Ministry of Science and Innovation (MCINN) through the CONSOLIDER (CSD2007-00050-II-PR4/07), MATRES (CGL2012-34221), and ExCirEs (CGL2011-24826) projects, and by the European Commission within the FP7 framework through the StratoClim project (Ref. 603557).es_ES
dc.language.isoenges_ES
dc.publisherInstitute of Physics Publishinges_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.subjectClimate change projectionses_ES
dc.subjectGlobal modelses_ES
dc.subjectFuture solar minimumes_ES
dc.titleThe impact of a future solar minimum on climate change projections in the Northern Hemispherees_ES
dc.typeArtículoes_ES
dc.identifier.doi10.1088/1748-9326/11/3/034015-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1088/1748-9326/11/3/034015es_ES
dc.identifier.e-issn1748-9326-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
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