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dc.contributor.authorTimmermans, Joris
dc.contributor.authorSu, Zhongbo
dc.contributor.authorPardo Gómez, Nuria 
dc.contributor.authorSánchez Gómez, María Luisa 
dc.contributor.authorPérez Bartolomé, Isidro Alberto 
dc.contributor.authorGarcía Pérez, María Ángeles 
dc.date.accessioned2024-02-02T08:59:38Z
dc.date.available2024-02-02T08:59:38Z
dc.date.issued2014
dc.identifier.citationAgricultural and Forest Meteorology 195–196 (2014) 132–142es
dc.identifier.issn0168-1923es
dc.identifier.urihttps://uvadoc.uva.es/handle/10324/65562
dc.descriptionProducción Científicaes
dc.description.abstractThis paper focuses on calculating Evaporative Fraction (EF) and energy balance components, applying theSurface Energy Balance System (SEBS) model combined with remote sensing products and meteorologicaldata over an agricultural rotating cropland from 2008 to 2011. The model is validated by comparingSEBS results with observed EF and surface fluxes obtained using an Eddy Covariance (EC) techniquetogether with meteorological instrumentation. Three different approaches of the model are evaluated:SEBS-0 (original algorithm), SEBS–SM (algorithm modified with soil moisture), and SEBS–NDVI (SEBS-0 modified with the Normalized Difference Vegetation Index – NDVI – and the surface temperature –Tsurf). Based on current knowledge of the close relationship between EF and NDVI, a modified SEBS-0algorithm, SEBS–NDVI, is proposed in this study. This new approach is developed so as to improve resultsfor EF and latent heat flux (LE), and this paper presents the results of all three SEBS approaches used inthis study. Modelled Rnis found to be in good agreement with observed data (R2= 0.75), although SEBS-calculated G gave less satisfactory results (R2= 0.38) and its seasonal dynamics shows discrepancies withobserved data. An evaluation of SEBS-0 shows a clear underestimation of H (R2= 0.54) and a markedoverestimation of EF and LE. Comparison with ground-based data yielded the best correlation applyingSEBS–NDVI, avoiding overestimation of EF and LE obtained with SEBS-0 and SEBS–SM. Results show thatthe proposed SEBS–NDVI, using a scale factor related to NDVI and Tsurf, is able to reproduce satisfactorilythe EF (R2= 0.65) and LE (R2= 0.70) seasonal pattern better than the two previous approaches for ourstudy plot.es
dc.format.mimetypeapplication/pdfes
dc.language.isospaes
dc.publisherElsevier B.V.es
dc.rights.accessRightsinfo:eu-repo/semantics/restrictedAccesses
dc.subject.classificationSurface Energy Balance System (SEBS)es
dc.subject.classificationRemote sensinges
dc.subject.classificationEnergy balancees
dc.subject.classificationEddy Covariancees
dc.subject.classificationEvaporative Fractiones
dc.subject.classificationNormalized Difference Vegetation Indexaes
dc.titleSEBS validation in a Spanish rotating cropes
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© 2014 Elsevier B.V. All rights reservedes
dc.identifier.doi10.1016/j.agrformet.2014.05.007es
dc.relation.publisherversionhttps://doi.org/10.1016/j.agrformet.2014.05.007es
dc.identifier.publicationfirstpage132es
dc.identifier.publicationlastpage142es
dc.identifier.publicationtitleAgricultural and Forest Meteorologyes
dc.identifier.publicationvolume195-196es
dc.peerreviewedSIes
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones


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