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hal.structure.identifierPeking University [Beijing]
dc.contributor.authorTAO, Shengli
hal.structure.identifierSouth China Normal University
dc.contributor.authorAO, Zurui
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorWIGNERON, Jean-Pierre
hal.structure.identifierCalifornia Institute of Technology [CALTECH]
dc.contributor.authorSAATCHI, Sassan
hal.structure.identifierLaboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] [LSCE]
dc.contributor.authorCIAIS, Philippe
hal.structure.identifierEvolution et Diversité Biologique [EDB]
dc.contributor.authorCHAVE, Jérôme
hal.structure.identifierCentre d'études spatiales de la biosphère [CESBIO]
dc.contributor.authorLE TOAN, Thuy
hal.structure.identifierLaboratoire sciences et technologies de l'information géographique [LaSTIG]
dc.contributor.authorFRISON, Pierre-Louis
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorHU, Xiaomei
hal.structure.identifierLawrence Berkeley National Laboratory [Berkeley] [LBNL]
dc.contributor.authorCHEN, Chi
hal.structure.identifierSouthwest University [Chongqing]
dc.contributor.authorFAN, Lei
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorWANG, Mengjia
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorZHU, Jiangling
hal.structure.identifierTianjin University of Science and Technology [TUST]
dc.contributor.authorZHAO, Xia
hal.structure.identifierZhengzhou University
dc.contributor.authorLI, Xiaojun
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorLIU, Xiangzhuo
hal.structure.identifierChinese Academy of Sciences [Beijing] [CAS]
dc.contributor.authorSU, Yanjun
hal.structure.identifierChinese Academy of Sciences [Beijing] [CAS]
dc.contributor.authorHU, Tianyu
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorGUO, Qinghua
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorWANG, Zhiheng
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorTANG, Zhiyao
hal.structure.identifierUniversity of New South Wales [Sydney] [UNSW]
dc.contributor.authorLIU, Yi
hal.structure.identifierPeking University [Beijing]
dc.contributor.authorFANG, Jingyun
dc.date.accessioned2024-04-08T11:44:13Z
dc.date.available2024-04-08T11:44:13Z
dc.date.issued2023-04-12
dc.identifier.issn1866-3508
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195143
dc.description.abstractSatellite radar backscatter contains unique information on land surface moisture, vegetation features, and surface roughness and has thus been used in a range of Earth science disciplines. However, there is no single global radar data set that has a relatively long wavelength and a decades-long time span. We here provide the first long-term (since 1992), high-resolution ( similar to 8 :9 km instead of the commonly used similar to 25 km resolution) monthly satellite radar backscatter data set over global land areas, called the long-term, high-resolution scatterometer (LHScat) data set, by fusing signals from the European Remote Sensing satellite (ERS; 1992-2001; C-band; 5.3 GHz), Quick Scatterometer (QSCAT, 1999-2009; Ku-band; 13.4 GHz), and the Advanced SCATterometer (ASCAT; since 2007; C-band; 5.255 GHz). The 6-year data gap between C-band ERS and ASCAT was filled by modelling a substitute C-band signal during 1999-2009 from Ku-band QSCAT signals and climatic information. To this end, we first rescaled the signals from different sensors, pixel by pixel. We then corrected the monthly signal differences between the C-band and the scaled Ku-band signals by modelling the signal differences from climatic variables (i.e. monthly precipitation, skin temperature, and snow depth) using decision tree regression.The quality of the merged radar signal was assessed by computing the Pearson r, root mean square error (RMSE), and relative RMSE (rRMSE) between the C-band and the corrected Ku-band signals in the overlapping years (1999-2001 and 2007-2009). We obtained high Pearson r values and low RMSE values at both the regional ( r >= 0 :92, RMSE <= 0.11 dB, and rRMSE <= 0.38) and pixel levels (median r across pixels >= 0.64, median RMSE <= 0.34 dB, and median rRMSE <= 0.88), suggesting high accuracy for the data-merging procedure. The merged radar signals were then validated against the European Space Agency (ESA) ERS-2 data, which provide observations for a subset of global pixels until 2011, even after the failure of on-board gyroscopes in 2001. We found highly concordant monthly dynamics between the merged radar signals and the ESA ERS-2 signals, with regional Pearson r values ranging from 0.79 to 0.98. These results showed that our merged radar data have a consistent C-band signal dynamic.The LHScat data set (https://doi.org/10.6084/m9.figshare.20407857; Tao et al., 2023) is expected to advance our understanding of the long-term changes in, e.g., global vegetation and soil moisture with a high spatial resolution. The data set will be updated on a regular basis to include the latest images acquired by ASCAT and to include even higher spatial and temporal resolutions.
dc.description.sponsorshipCEnter of the study of Biodiversity in Amazonia
dc.description.sponsorshipTowards a Unified theory of biotic Interactions: the roLe of environmental
dc.language.isoen
dc.publisherCopernicus Publications
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.title.enA global long-term, high-resolution satellite radar backscatter data record (1992-2022+): merging C-band ERS/ASCAT and Ku-band QSCAT
dc.typeArticle de revue
dc.typeData paper
dc.identifier.doi10.5194/essd-15-1577-2023
dc.subject.halSciences de l'environnement
bordeaux.journalEarth System Science Data
bordeaux.page1577-1596
bordeaux.volume15
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue4
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-04095888
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-04095888v1
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