dc.contributor.author | Brands, Swen Franz | |
dc.contributor.author | García Manzanas, Rodrigo | |
dc.contributor.author | Gutiérrez Llorente, José Manuel | |
dc.contributor.author | Cohen, Judah L. | |
dc.contributor.other | Universidad de Cantabria | es_ES |
dc.date.accessioned | 2019-12-05T11:29:03Z | |
dc.date.available | 2019-12-05T11:29:03Z | |
dc.date.issued | 2012-06-15 | |
dc.identifier.issn | 0894-8755 | |
dc.identifier.issn | 1520-0442 | |
dc.identifier.other | CGL2010-21869 | es_ES |
dc.identifier.uri | http://hdl.handle.net/10902/17403 | |
dc.description.abstract | This 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.sponsorship | SB, 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.extent | 6 p. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | American Meteorological Society | es_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.source | Journal of Climate, 2012,
25(12), 4023-4028 | es_ES |
dc.subject.other | Europe | es_ES |
dc.subject.other | Teleconnections | es_ES |
dc.subject.other | Hydrology | es_ES |
dc.subject.other | Snow cover | es_ES |
dc.subject.other | Seasonal forecasting | es_ES |
dc.subject.other | Statistical forecasting | es_ES |
dc.title | Seasonal predictability of wintertime precipitation in Europe using the snow advance index | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.relation.publisherVersion | https://doi.org/10.1175/JCLI-D-12-00083.1 | es_ES |
dc.rights.accessRights | openAccess | es_ES |
dc.identifier.DOI | 10.1175/JCLI-D-12-00083.1 | |
dc.type.version | publishedVersion | es_ES |