Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.11765/11743
Water vapor radiative effects on short-wave radiation in Spain
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dc.contributor.authorVaquero Martínez, Javieres_ES
dc.contributor.authorAntón, Manueles_ES
dc.contributor.authorOrtiz de Galisteo, José Pabloes_ES
dc.contributor.authorRomán, Robertoes_ES
dc.contributor.authorCachorro, Victoria E.es_ES
dc.date.accessioned2020-05-06T08:50:42Z-
dc.date.available2020-05-06T08:50:42Z-
dc.date.issued2018-
dc.identifier.citationAtmospheric Research. 2018, 205, p. 18-25es_ES
dc.identifier.issn0169-8095-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/11743-
dc.descriptionThis work was supported by the Spanish Ministry of Economy and Competitiveness through project CGL2014-56255-C2. Support from the Junta de Extremadura (Research Group Grant GR15137) is gratefully acknowledged. Work at the Universidad de Valladolid is supported by project CMT2015-66742-R. Work at the Universidad de Granada was supported by the Andalusia Regional Government (Project P12-RNM-2409) and the Spanish Ministry of Economy and Competitiveness and FEDER funds under the projects CGL2016-81092-R and “Juan de la Cierva-Formación” program (FJCI-2014-22052).es_ES
dc.description.abstractIn this work, water vapor radiative effect (WVRE) is studied by means of the Santa Barbara's Disort Radiative Transfer (SBDART) model, fed with integrated water vapor (IWV) data from 20 ground-based GPS stations in Spain. Only IWV data recorded during cloud-free days (selected using daily insolation data) were used in this study. Typically, for SZA = 60.0 ± 0.5° WVRE values are around − 82 and − 66 Wm−2 (first and third quartile), although it can reach up − 100 Wm−2 or decrease to − 39 Wm−2. A power dependence of WVRE on IWV and cosine of solar zenith angle (SZA) was found by an empirical fit. This relation is used to determine the water vapor radiative efficiency (WVEFF = ∂WVRE/∂IWV). Obtained WVEFF values range from − 9 and 0 Wm−2 mm−1 (− 2.2 and 0% mm−1 in relative terms). It is observed that WVEFF decreases as IWV increases, but also as SZA increases. On the other hand, when relative WVEFF is calculated from normalized WVRE, an increase of SZA results in an increase of relative WVEFF. Heating rates were also calculated, ranging from 0.2 Kday−1 to 1.7 Kday−1. WVRE was also calculated at top of atmosphere, where values ranged from 4 Wm−2 to 37 Wm−2es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.subjectShort-wavees_ES
dc.subjectRadiative effectes_ES
dc.subjectRadiative efficiencyes_ES
dc.subjectWater vapores_ES
dc.subjectIWVes_ES
dc.titleWater vapor radiative effects on short-wave radiation in Spaines_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://dx.doi.org/10.1016/j.atmosres.2018.02.001es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Appears in Collections:Artículos científicos 2015-2018


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