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dc.contributor.authorGhilain, Nicolas
dc.contributor.authorArboleda, Alirio
dc.contributor.authorSepulcre-Canto, Guadalupe
dc.contributor.authorBatelaan, Okke
dc.contributor.authorArdö, Jonas
dc.contributor.authorGellens-Meulenberghs, Françoise
dc.contributor.editorLoew, Alexander
dc.coverage.spatialEurope, Africaen_US
dc.coverage.temporal2004-2012en_US
dc.date2012-08-08
dc.date.accessioned2019-05-21T15:17:52Z
dc.date.available2019-05-21T15:17:52Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/7281
dc.descriptionMonitoring evapotranspiration over land is highly dependent on the surface state and vegetation dynamics. Data from spaceborn platforms are desirable to complement estimations from land surface models. The success of daily evapotranspiration monitoring at continental scale relies on the availability, quality and continuity of such data. The biophysical variables derived from SEVIRI on board the geostationary satellite Meteosat Second Generation (MSG) and distributed by the Satellite Application Facility on Land surface Analysis (LSA-SAF) are particularly interesting for such applications, as they aimed at providing continuous and consistent daily time series in near-real time over Africa, Europe and South America. In this paper, we compare them to monthly vegetation parameters from a database commonly used in numerical weather predictions (ECOCLIMAP-I), showing the benefits of the new daily products in detecting the spatial and temporal (seasonal and inter-annual) variability of the vegetation, especially relevant over Africa. We propose a method to handle Leaf Area Index (LAI) and Fractional Vegetation Cover (FVC) products for evapotranspiration monitoring with a land surface model at 3–5 km spatial resolution. The method is conceived to be applicable for near-real time processes at continental scale and relies on the use of a land cover map. We assess the impact of using LSA-SAF biophysical variables compared to ECOCLIMAP-I on evapotranspiration estimated by the land surface model H-TESSEL. Comparison with in-situ observations in Europe and Africa shows an improved estimation of the evapotranspiration, especially in semi-arid climates. Finally, the impact on the land surface modelled evapotranspiration is compared over a north–south transect with a large gradient of vegetation and climate in Western Africa using LSA-SAF radiation forcing derived from remote sensing. Differences are highlighted. An evaluation against remote sensing derived land surface temperature shows an improvement of the evapotranspiration simulations.en_US
dc.languageengen_US
dc.publisherCopernicus Publicationsen_US
dc.titleImproving evapotranspiration in a land surface model using biophysical variables derived from MSG/SEVIRI satelliteen_US
dc.typeArticleen_US
dc.subject.frascatiEarth and related Environmental sciencesen_US
dc.audienceScientificen_US
dc.subject.freeevapotranspiration, vegetation, satellitesen_US
dc.source.titleHydrology and Earth System Sciencesen_US
dc.source.volume16en_US
dc.source.issue8en_US
dc.source.page2567– 2583en_US
dc.relation.projectEUMETSAT LSA-SAF CDOP2en_US
dc.relation.projectPROBA-VETen_US
Orfeo.peerreviewedYesen_US
dc.identifier.doi10.5194/hess-16-2567-2012
dc.relation.belspo-projectPROBA-VETen_US
dc.relation.belspo-projectLSA-SAF (contract e15066)en_US


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