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dc.contributor.author | Timmermans, Joris | |
dc.contributor.author | Su, Zhongbo | |
dc.contributor.author | Pardo Gómez, Nuria | |
dc.contributor.author | Sánchez Gómez, María Luisa | |
dc.contributor.author | Pérez Bartolomé, Isidro Alberto | |
dc.contributor.author | García Pérez, María Ángeles | |
dc.date.accessioned | 2024-02-02T08:59:38Z | |
dc.date.available | 2024-02-02T08:59:38Z | |
dc.date.issued | 2014 | |
dc.identifier.citation | Agricultural and Forest Meteorology 195–196 (2014) 132–142 | es |
dc.identifier.issn | 0168-1923 | es |
dc.identifier.uri | https://uvadoc.uva.es/handle/10324/65562 | |
dc.description | Producción Científica | es |
dc.description.abstract | This 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.mimetype | application/pdf | es |
dc.language.iso | spa | es |
dc.publisher | Elsevier B.V. | es |
dc.rights.accessRights | info:eu-repo/semantics/restrictedAccess | es |
dc.subject.classification | Surface Energy Balance System (SEBS) | es |
dc.subject.classification | Remote sensing | es |
dc.subject.classification | Energy balance | es |
dc.subject.classification | Eddy Covariance | es |
dc.subject.classification | Evaporative Fraction | es |
dc.subject.classification | Normalized Difference Vegetation Indexa | es |
dc.title | SEBS validation in a Spanish rotating crop | es |
dc.type | info:eu-repo/semantics/article | es |
dc.rights.holder | © 2014 Elsevier B.V. All rights reserved | es |
dc.identifier.doi | 10.1016/j.agrformet.2014.05.007 | es |
dc.relation.publisherversion | https://doi.org/10.1016/j.agrformet.2014.05.007 | es |
dc.identifier.publicationfirstpage | 132 | es |
dc.identifier.publicationlastpage | 142 | es |
dc.identifier.publicationtitle | Agricultural and Forest Meteorology | es |
dc.identifier.publicationvolume | 195-196 | es |
dc.peerreviewed | SI | es |
dc.type.hasVersion | info:eu-repo/semantics/publishedVersion | es |
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