Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/105891
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorČunderlík, R-
dc.creatorTenzer, R-
dc.creatorMacák, M-
dc.creatorZahorec, P-
dc.creatorPapčo, J-
dc.creatorAbabio, AN-
dc.date.accessioned2024-04-23T04:32:03Z-
dc.date.available2024-04-23T04:32:03Z-
dc.identifier.issn2081-9919-
dc.identifier.urihttp://hdl.handle.net/10397/105891-
dc.language.isoenen_US
dc.publisherWalter de Gruyter GmbHen_US
dc.rights© 2023 the author(s), published by De Gruyter. This work is licensed under the Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Čunderlík, Robert, Tenzer, Robert, Macák, Marek, Zahorec, Pavol, Papčo, Juraj and Nsiah Ababio, Albertini. "A detailed quasigeoid model of the Hong Kong territories computed by applying a finite-element method of solving the oblique derivative boundary-value problem" Journal of Geodetic Science, vol. 13, no. 1, 2023, pp. 20220153 is available at https://doi.org/10.1515/jogs-2022-0153.en_US
dc.subjectBoundary-value problemen_US
dc.subjectFinite-element method, gravityen_US
dc.subjectHeightsen_US
dc.subjectLevellingen_US
dc.subject(Quasi)geoiden_US
dc.subjectVertical geodetic controlen_US
dc.titleA detailed quasigeoid model of the Hong Kong territories computed by applying a finite-element method of solving the oblique derivative boundary-value problemen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume13-
dc.identifier.issue1-
dc.identifier.doi10.1515/jogs-2022-0153-
dcterms.abstractNew gravity and precise levelling measurements have been performed throughout the Hong Kong territories to modernize a vertical geodetic datum that is currently realized by heights of levelling benchmarks defined in the Hong Kong Principal Datum (HKPD). Modernization of the HKPD involved delivering various products, including new detailed geoid and quasigeoid models and newly determined orthometric and normal heights of levelling benchmarks. In this study, we present the result of gravimetric quasigeoid modelling. The method used to compute a detailed gravimetric quasigeoid model is based on the finite-element method to solve the geodetic boundary-value problem with oblique derivative boundary conditions considered directly at computational nodes on the discretized Earth’s topography. The result of a gravimetric quasigeoid modelling shows a good agreement with a geometric quasigeoid model at the Global Navigation Satellite System (GNSS)-levelling benchmarks. The standard deviation of differences between the gravimetric and geometric quasigeoid heights of ±3.3 cm is compatible with the expected accuracy of gravity, levelling, and GNSS measurements.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geodetic science, Jan. 2023, v. 13, no. 1, 20220153-
dcterms.isPartOfJournal of geodetic science-
dcterms.issued2023-01-
dc.identifier.scopus2-s2.0-85153510363-
dc.identifier.eissn2081-9943-
dc.identifier.artn20220153-
dc.description.validate202404 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceRGCen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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