Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/100774
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorChen, Qen_US
dc.creatorShen, Yen_US
dc.creatorChen, Wen_US
dc.creatorZhang, Xen_US
dc.creatorHsu, Hen_US
dc.date.accessioned2023-08-11T03:13:22Z-
dc.date.available2023-08-11T03:13:22Z-
dc.identifier.issn0949-7714en_US
dc.identifier.urihttp://hdl.handle.net/10397/100774-
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.rights© Springer-Verlag Berlin Heidelberg 2016en_US
dc.rightsThis version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature’s AM terms of use(https://www.springernature.com/gp/open-research/policies/accepted-manuscript-terms), but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: http://dx.doi.org/10.1007/s00190-016-0889-6.en_US
dc.subjectGRACEen_US
dc.subjectMonthly gravity field modelen_US
dc.subjectNon-conservative accelerationen_US
dc.subjectSatellite geodesyen_US
dc.titleAn improved GRACE monthly gravity field solution by modeling the non-conservative acceleration and attitude observation errorsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage503en_US
dc.identifier.epage523en_US
dc.identifier.volume90en_US
dc.identifier.issue6en_US
dc.identifier.doi10.1007/s00190-016-0889-6en_US
dcterms.abstractThe main contribution of this study is to improve the GRACE gravity field solution by taking errors of non-conservative acceleration and attitude observations into account. Unlike previous studies, the errors of the attitude and non-conservative acceleration data, and gravity field parameters, as well as accelerometer biases are estimated by means of weighted least squares adjustment. Then we compute a new time series of monthly gravity field models complete to degree and order 60 covering the period Jan. 2003 to Dec. 2012 from the twin GRACE satellites’ data. The derived GRACE solution (called Tongji-GRACE02) is compared in terms of geoid degree variances and temporal mass changes with the other GRACE solutions, namely CSR RL05, GFZ RL05a, and JPL RL05. The results show that (1) the global mass signals of Tongji-GRACE02 are generally consistent with those of CSR RL05, GFZ RL05a, and JPL RL05; (2) compared to CSR RL05, the noise of Tongji-GRACE02 is reduced by about 21 % over ocean when only using 300 km Gaussian smoothing, and 60 % or more over deserts (Australia, Kalahari, Karakum and Thar) without using Gaussian smoothing and decorrelation filtering; and (3) for all examples, the noise reductions are more significant than signal reductions, no matter whether smoothing and filtering are applied or not. The comparison with GLDAS data supports that the signals of Tongji-GRACE02 over St. Lawrence River basin are close to those from CSR RL05, GFZ RL05a and JPL RL05, while the GLDAS result shows the best agreement with the Tongji-GRACE02 result.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geodesy, June 2016, v. 90, no. 6, p. 503-523en_US
dcterms.isPartOfJournal of geodesyen_US
dcterms.issued2016-06-
dc.identifier.scopus2-s2.0-84967321443-
dc.identifier.eissn1432-1394en_US
dc.description.validate202305 bckw-
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberLSGI-0442-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; National key Basic Research Program of China; State Key Laboratory of Geodesy and Earth’s Dynamics; State Key Laboratory of Geo-information Engineeringen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS6643058-
dc.description.oaCategoryGreen (AAM)en_US
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