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dc.contributor.authorJordà, Gabriel
dc.contributor.authorGomis, Damia
dc.contributor.authorTalone, Marco
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Teoria del Senyal i Comunicacions
dc.date.accessioned2011-09-14T12:27:29Z
dc.date.available2011-09-14T12:27:29Z
dc.date.created2011-03
dc.date.issued2011-03
dc.identifier.citationJordà, G.; Gomis, D.; Talone, M. The SMOS L3 mapping algorithm for sea surface salinity. "IEEE transactions on geoscience and remote sensing", Març 2011, vol. 49, núm. 3, p. 1032-1051.
dc.identifier.issn0196-2892
dc.identifier.urihttp://hdl.handle.net/2117/13194
dc.description.abstractThe Soil Moisture and Ocean Salinity (SMOS) mission launched in November 2009 will provide, for the first time, satellite observations of sea surface salinity (SSS). At level 3 (L3) of the SMOS processing chain, the large amount of SSS data obtained by the satellite will be summarized in gridded products with the aim of synthesizing the information and reducing the error of individual SSS observations. In this paper, we present the algorithm adopted by the CP34 SMOS processing center to generate the SMOS L3 products and discuss the choices adopted. The algorithm is based on optimal statistical interpolation. This method needs the following: 1) the prescription of a background field; 2) a prefiltering procedure to reduce the data set size; 3) the definition of a suitable correlation model; and 4) the characterization of the observational error statistics. For the present initial stage, a monthly climatology is chosen as the best background field. The spatiotemporal correlations between the departures from the climatology are described using a bivariate Gaussian function. The correlation model parameters are obtained by fitting the function to the realistic ocean model data. The sensitivity experiments show that an accurate correlation model that permits local variations in the correlation parameters is the best option. The observational error statistics (bias, variance, and correlation) are addressed from the results of the SMOS level-2 processor simulator. Finally, several sensitivity experiments show that a bad prescription of observational errors in the L3 algorithm does result in a dramatic impact on the generation of L3 products.
dc.format.extent20 p.
dc.language.isoeng
dc.publisherIEEE Press. Institute of Electrical and Electronics Engineers
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Oceanografia
dc.subject.lcshSoil Moisture and Ocean Salinity satellite
dc.subject.lcshSMOS
dc.subject.lcshMicrowave radiometry
dc.subject.lcshSea salinity
dc.titleThe SMOS L3 mapping algorithm for sea surface salinity
dc.typeArticle
dc.subject.lemacAigua de mar -- Salinitat
dc.subject.lemacRadiometria
dc.identifier.doi10.1109/TGRS.2010.2068551
dc.description.peerreviewedPeer Reviewed
dc.rights.accessRestricted access - publisher's policy
drac.iddocument5412694
dc.description.versionPostprint (published version)
upcommons.citation.authorJordà, G.; Gomis, D.; Talone, M.
upcommons.citation.publishedtrue
upcommons.citation.publicationNameIEEE transactions on geoscience and remote sensing
upcommons.citation.volume49
upcommons.citation.number3
upcommons.citation.startingPage1032
upcommons.citation.endingPage1051


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