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dc.contributor.authorBrands, Swen Franz 
dc.contributor.authorGarcía Manzanas, Rodrigo 
dc.contributor.authorGutiérrez Llorente, José Manuel
dc.contributor.authorCohen, Judah L.
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2019-12-05T11:29:03Z
dc.date.available2019-12-05T11:29:03Z
dc.date.issued2012-06-15
dc.identifier.issn0894-8755
dc.identifier.issn1520-0442
dc.identifier.otherCGL2010-21869es_ES
dc.identifier.urihttp://hdl.handle.net/10902/17403
dc.description.abstractThis study tests the applicability of Eurasian snow cover increase in October, as described by the recently published snow advance index (SAI), for forecasting December–February precipitation totals in Europe. On the basis of a classical correlation analysis, global significance was obtained and locally significant correlation coefficients of up to 0.89 and 20.78 were found for the Iberian Peninsula and southern Norway, respectively. For a more robust assessment of these results, a linear regression approach is followed to hindcast the precipitation sums in a 1-yr-out cross-validation framework, using the SAI as the only predictor variable. With this simple empirical approach, local-scale precipitation could be reproduced with a correlation of up to 0.84 and 0.71 for the Iberian Peninsula and southern Norway, respectively, while catchment aggregations on the Iberian Peninsula could be hindcast with a correlation of up to 0.73. These findings are confirmed when repeating the hindcast approach to a degraded but much longer version of the SAI. With the recommendation to monitor the robustness of these results as the sample size of the SAI increases, the authors encourage its use for the purpose of seasonal forecasting in southern Norway and the Iberian Peninsula, where general circulation models are known to perform poorly for the variable in question.es_ES
dc.description.sponsorshipSB, RM, and JMG acknowledge funding from the CICYT Project CGL2010-21869 and from QWeCI (EU Grant 243964) and the CSIC JAE-PREDOC program. JC is supported by the National Science Foundation Grants ARC-0909459 and ARC-0909457, and NOAA Grant NA10OAR4310163. The authors are thankful for the helpful comments of the three anonymous reviewers and acknowledge the E-OBS dataset from the ENSEMBLES project (http://ensembles-eu.metoffice.com/) as well the ECA&D(http:// eca.knmi.nl/) and AEMET station datasets.es_ES
dc.format.extent6 p.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Meteorological Societyes_ES
dc.rights© 2012 American Meteorological Society. AMS´s Full Copyright Notice: https://www.ametsoc.org/ams/index.cfm/publications/authors/journal-and-bams-authors/author-resources/copyright-information/copyright-policy/es_ES
dc.sourceJournal of Climate, 2012, 25(12), 4023-4028es_ES
dc.subject.otherEuropees_ES
dc.subject.otherTeleconnectionses_ES
dc.subject.otherHydrologyes_ES
dc.subject.otherSnow coveres_ES
dc.subject.otherSeasonal forecastinges_ES
dc.subject.otherStatistical forecastinges_ES
dc.titleSeasonal predictability of wintertime precipitation in Europe using the snow advance indexes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1175/JCLI-D-12-00083.1es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1175/JCLI-D-12-00083.1
dc.type.versionpublishedVersiones_ES


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