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dc.contributor.authorVicente Serrano, Sergio M.-
dc.contributor.authorLópez-Moreno, Juan I.-
dc.contributor.authorVega-Rodríguez, M. Isabel-
dc.contributor.authorBeguería, Santiago-
dc.contributor.authorCuadrat, José María-
dc.date.accessioned2010-08-04T07:39:39Z-
dc.date.available2010-08-04T07:39:39Z-
dc.date.issued2010-05-
dc.identifier.citationVicente SM, López-Moreno JI, Vega-Rodríguez MI, Beguería S, Cuadrat JM. Comparison of regression techniques for mapping fog frequency: application to the Aragón region (northeast Spain). International Journal of Climatology 30(6): 935 - 945 (2010)en_US
dc.identifier.issn0899-8418-
dc.identifier.urihttp://hdl.handle.net/10261/26783-
dc.description28 páginas,, 4 tablas, 7 figuras. The definitive version is available at: http://www3.interscience.wiley.com/journal/4735/homeen_US
dc.description.abstractWe compare different spatial interpolation techniques in mapping the monthly frequency of fogs in the Aragón region (northeast Spain). The local and spatially complex nature of the fogs makes them more difficult to map than other climatic variables such as precipitation and temperature. We found clear seasonal differences in the quality of the obtained maps. The localized nature of spring and summer fogs, mainly restricted to valley bottoms in mountainous areas, gives rise to several limitations. The modelling of fog frequency is more complex than that of other climate variables; to improve the model predictions, it is necessary to consider topographic variables that simulate the terrain structure. Moreover, the highly complex nature of the relationship between fog frequency and terrain means that simple linear models perform poorly in accounting for the role of geographic and topographic variables in determining the spatial distribution of fog frequency. The inclusion of non-linear relationships between fog frequency and terrain variables in the models following a general additive model (GAM) procedure leads to an improvement in model performance because the flexibility of GAMs enables the inclusion of non-linear relationships and the generation of response-curve shapes that detail the exact relationship between the dependent variable and predictors throughout the entire range of the variable.en_US
dc.description.sponsorshipThis work has been supported by the following research projects: CGL2005-04508/BOS (financed by the Spanish Commission of Science and Technology and FEDER), PIP176/2005 (financed by the Aragón Government), and “Programa de grupos de investigación consolidados” (BOA 48 of 20-04-2005), also financed by the Aragón Government.en_US
dc.format.extent357629 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoengen_US
dc.publisherJohn Wiley & Sonsen_US
dc.rightsopenAccessen_US
dc.subjectFog frequencyen_US
dc.subjectFog mappingen_US
dc.subjectInterpolationen_US
dc.subjectOrdinary least squares regressionen_US
dc.subjectSplinesen_US
dc.subjectGeneral additive modelsen_US
dc.subjectNon-linearityen_US
dc.subjectAragónen_US
dc.titleComparison of regression techniques for mapping fog frequency: application to the Aragón region (northeast Spain)en_US
dc.typeartículoen_US
dc.identifier.doi10.1002/joc.1935-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttp://dx.doi.org/10.1002/joc.1935en_US
dc.identifier.e-issn1097-0088-
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.openairetypeartículo-
item.languageiso639-1en-
item.grantfulltextopen-
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