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hal.structure.identifierCatholic University of Leuven = Katholieke Universiteit Leuven [KU Leuven]
dc.contributor.authorVINCENT, Frederike
hal.structure.identifierCatholic University of Leuven = Katholieke Universiteit Leuven [KU Leuven]
dc.contributor.authorMAERTENS, Michiel
hal.structure.identifierCatholic University of Leuven = Katholieke Universiteit Leuven [KU Leuven]
dc.contributor.authorBECHTOLD, Michel
hal.structure.identifierInstituto de Matemática Aplicada San Luis [IMASL]
dc.contributor.authorJOBBAGY, Esteban
hal.structure.identifierNASA Goddard Space Flight Center [GSFC]
dc.contributor.authorREICHLE, Rolf
hal.structure.identifierUniversité Catholique de Louvain = Catholic University of Louvain [UCL]
dc.contributor.authorVANACKER, Veerle
hal.structure.identifierUniversity of California [Irvine] [UC Irvine]
hal.structure.identifierUniversity of Amsterdam [Amsterdam] = Universiteit van Amsterdam [UvA]
dc.contributor.authorVRUGT, Jasper
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorJ.-P., Wigneron
hal.structure.identifierCatholic University of Leuven = Katholieke Universiteit Leuven [KU Leuven]
dc.contributor.authorDE LANNOY, Gabrielle
dc.date.accessioned2024-04-08T11:46:30Z
dc.date.available2024-04-08T11:46:30Z
dc.date.issued2022
dc.identifier.issn1939-1404
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195235
dc.description.abstractEnThe Dry Chaco in South America is a semi-arid ecoregion prone to dryland salinization. In this region, we investigated coarse-scale surface soil moisture (SM), soil temperature, soil salinity, and vegetation, using L-band microwave brightness temperature (T B) observations and retrievals from the soil moisture ocean salinity (SMOS) and soil moisture active passive satellite missions, Catchment land surface model (CLSM) simulations, and in situ measurements within 26 sampled satellite pixels. Across these 26 sampled pixels, the satellite-based SM outperformed CLSM SM when evaluated against field data, and the forward L-band T B simulations derived from in situ SM and soil temperature performed better than those derived from CLSM estimates when evaluated against SMOS T B observations. The surface salinity for the sampled pixels was on average only 4 mg/g and only locally influenced the T B simulations, when including salinity in the dielectric mixing model of the forward radiative transfer model (RTM) simulations. To explore the potential of retrieving salinity together with other RTM parameters to optimize T B simulations over the entire Dry Chaco, the RTM was inverted using 10 years of multiangular SMOS T B data and constraints of CLSM SM and soil temperature. However, the latter modeled SM was not sufficiently accurate and
dc.language.isoen
dc.publisherIEEE
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subject.enL-band microwave
dc.subject.enland surface model
dc.subject.ensalinity
dc.subject.ensoil moisture
dc.subject.ensoil moisture active passive (SMAP)
dc.subject.ensoil moisture ocean salinity (SMOS)
dc.subject.ensoil temperature
dc.subject.envegetation
dc.title.enL-Band Microwave Satellite Data and Model Simulations Over the Dry Chaco to Estimate Soil Moisture, Soil Temperature, Vegetation, and Soil Salinity
dc.typeArticle de revue
dc.identifier.doi10.1109/jstars.2022.3193636
dc.subject.halSciences de l'environnement
bordeaux.journalIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
bordeaux.page6598 - 6614
bordeaux.volume15
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-03775504
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-03775504v1
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