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dc.contributor.authorGómez, Mario
dc.contributor.authorAusín, M. Concepción
dc.contributor.authorDomínguez Álvarez, María Carmen 
dc.date.accessioned2021-06-01T11:17:04Z
dc.date.available2021-06-01T11:17:04Z
dc.date.issued2018
dc.identifier.citationGómez, M., Ausín, M.C. & Domínguez, M.C.(2018) Vine copula models for predicting water flow discharge at King George Island, Antarctica. Stoch Environ Res Risk Assess 32, 2787–2807 . https://doi.org/10.1007/s00477-018-1599-9es_ES
dc.identifier.issn1436-3240
dc.identifier.urihttp://hdl.handle.net/10366/146618
dc.description.abstract[EN]In order to understand the behavior of the glaciers, their mass balance should be studied. The loss of water produced by melting, known as glacier discharge, is one of the components of this mass balance. In this paper, a vine copula structure is proposed to model the multivariate and nonlinear dependence among the glacier discharge and other related meteorological variables such as temperature, humidity, solar radiation and precipitation. The multivariate distribution of these variables is expressed as a mixture of four components according to the presence or not of positive discharge and/or positive precipitation. Then, each of the four subgroups is modelled with a vine copula. The conditional probability of zero discharge for given meteorological conditions is obtained from the proposed joint distribution. Moreover, the structure of the vine copula allows us to derive the conditional distribution of the glacier discharge for the given meteorological conditions. Three different prediction methods for the values of the discharge are used and compared. The proposed methodology is applied to a large database collected since 2002 by the GLACKMA association from a measurement station located in the King George Island in the Antarctica. Seasonal effects are included by using different parameters for each season. We have found that the proposed vine copula model outperforms a previous work where we only used the temperature to predict the glacier discharge using a time-varying bivariate copula.es_ES
dc.language.isoenges_ES
dc.publisherSpringer Linkes_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectFinite mixtureses_ES
dc.subjectGlacier dischargees_ES
dc.subjectMeteorologicales_ES
dc.subjectPredictiones_ES
dc.subjectVine copulaes_ES
dc.titleVine copula models for predicting water flow discharge at King George Island, Antarcticaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1007/s00477-018-1599-9es_ES
dc.subject.unesco12 Matemáticases_ES
dc.identifier.doi10.1007/s00477-018-1599-9
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.essn1436-3259
dc.journal.titleStochastic Environmental Research and Risk Assessmentes_ES
dc.volume.number32es_ES
dc.issue.number10es_ES
dc.page.initial2787es_ES
dc.page.final2807es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internacional