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hal.structure.identifierUniversity of Stuttgart
dc.contributor.authorTOURIAN, Mohammad
hal.structure.identifierUniversity of Stuttgart
dc.contributor.authorSAEMIAN, Peyman
hal.structure.identifierHohai University
dc.contributor.authorFERREIRA, Vagner
hal.structure.identifierUniversity of Stuttgart
dc.contributor.authorSNEEUW, Nico
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorFRAPPART, Frédéric
hal.structure.identifierLaboratoire d'études en Géophysique et océanographie spatiales [LEGOS]
hal.structure.identifierUniversity of Brasilia [Brazil] [UnB]
dc.contributor.authorPAPA, Fabrice
dc.date.accessioned2024-04-08T11:42:41Z
dc.date.available2024-04-08T11:42:41Z
dc.date.issued2023-09
dc.identifier.issn0034-4257
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195078
dc.description.abstractEnThe GRACE and GRACE-FO satellite missions provide mass variations as a fundamentally new observation type for a broad spectrum of novel applications in Earth science disciplines, including oceanography, geophysics, hydrology, and hydrometeorology. Despite all the key findings in hydrology, the utility of GRACE-derived Terrestrial Water Storage Anomaly (TWSA) and its time derivative Terrestrial Water Storage Flux (TWSF) have mainly been limited to large catchments due to their coarse spatial resolution. Here, we propose a method to downscale TWSF by incorporating available finer-resolution data. We determine the downscaled TWSF and its uncertainty within a proposed Bayesian framework by incorporating the fine-scale data of TWSF and Soil Moisture Change (SMC) from different available sources. For the Bayesian ingredients, we rely on GRACE data to obtain the prior and rely on copula models to obtain nonparametric likelihood functions based on the statistical relationship between GRACE TWSF with fine-scale TWSF data and SMC. We apply our method to the Amazon Basin and assess the performances of our products from various fine-scale input datasets of TWSFs and SMCs. Given the lack of ground truth for TWSF, we validate our results against space-based Surface Water Storage Change (SWSC) in the Amazon river system and also against the Vertical Crustal Displacements Rate (VCDR) observed by the Global Positioning System (GPS). Overall, the results show that the proposed method is able to estimate a downscaled TWSF, which is informed by GRACE and fine-scale data. Validation shows that our downscaled products are better anticorrelated with VCDR (−0.81) than fine-scale TWSF (−0.73) and show a mean relative RMSE of 26% with SWSC versus 70% for fine-scale TWSF. The proposed methodology can be extended to other coarse scale datasets, which are crucial for hydrological application at regional and local scales.
dc.language.isoen
dc.publisherElsevier
dc.subject.enCopula
dc.subject.enBayesian framework
dc.subject.enDownscaling
dc.subject.enGRACE
dc.subject.enTerrestrial water storage flux
dc.title.enA copula-supported Bayesian framework for spatial downscaling of GRACE-derived terrestrial water storage flux
dc.typeArticle de revue
dc.identifier.doi10.1016/j.rse.2023.113685
dc.subject.halSciences de l'environnement
bordeaux.journalRemote Sensing of Environment
bordeaux.page113685
bordeaux.volume295
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-04214595
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-04214595v1
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