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                <term xml:lang="fr">BASSIN DE L'ADOUR</term>
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              <classCode scheme="halDomain" n="sde">Environmental Sciences</classCode>
              <classCode scheme="vocinrae-old" n="BILAN HYDRIQUE">BILAN HYDRIQUE</classCode>
              <classCode scheme="vocinrae-old" n="MODELE PLUIE DEBIT">MODELE PLUIE DEBIT</classCode>
              <classCode scheme="vocinrae-old" n="ETAT DE SURFACE">ETAT DE SURFACE</classCode>
              <classCode scheme="vocinrae-old" n="WATER BALANCE">WATER BALANCE</classCode>
              <classCode scheme="vocinrae-old" n="CANOPY">CANOPY</classCode>
              <classCode scheme="vocinrae-old" n="SOIL WATER CONTENT">SOIL WATER CONTENT</classCode>
              <classCode scheme="vocinrae-old" n="RADAR">RADAR</classCode>
              <classCode scheme="vocinrae-old" n="IMAGE ANALYSIS">IMAGE ANALYSIS</classCode>
              <classCode scheme="vocinrae-old" n="CALIBRATION">CALIBRATION</classCode>
              <classCode scheme="vocinrae-old" n="RHIZOSPHERE">RHIZOSPHERE</classCode>
              <classCode scheme="vocinrae-old" n="RAINFALL RUNOFF MODEL">RAINFALL RUNOFF MODEL</classCode>
              <classCode scheme="vocinrae-old" n="COUVERT VEGETAL">COUVERT VEGETAL</classCode>
              <classCode scheme="vocinrae-old" n="INFRAROUGE THERMIQUE">INFRAROUGE THERMIQUE</classCode>
              <classCode scheme="vocinrae-old" n="HUMIDITE DU SOL">HUMIDITE DU SOL</classCode>
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              <p>Different studies have shown that several surface parameters important for the following of the soils hydric budget may be inferred from remote sensing. These variables may afterwards be assimilated in hydrological models to improve the simulation of the exchanges between soil and atmosphere and finally the waterflows over the catchments. The ways to infer vegetation parameters from remote sensing data, the calibration of the SAR data in terms of soil humidity and the methodology of estimating soil moisture in the surface layer from thermal infrared data are presented in this paper. Then, an example of their assimilation in an hydrological model on the Adour river basin is shown.</p>
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              <p>Différentes études ont montré que plusieurs paramètres de surface importants pour le suivi du bilan hydrique peuvent être déduits des données de télédétection. Ces variables peuvent être ensuite intégrées à des modèles hydrologiques qui cherchent à améliorer la simulation des échanges entre sol et atmosphère et finalement des écoulements sur les bassins versants. Cette communication présente la méthode pour déduire, des données de télédétection, les paramètres de végétation, ainsi que l'étalonnage, à partir des données d'infra-rouge thermique, des données radar SAR en termes d'humidité du sol et la méthodologie d'estimation de l'humidité de l'état de surface. Ensuite, on donne un exemple d'intégration de ces données dans un modèle hydrologique du bassin versant de l'Adour.</p>
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