Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/89115
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorShen, Y-
dc.creatorChen, Q-
dc.creatorXu, H-
dc.date.accessioned2021-02-04T02:39:28Z-
dc.date.available2021-02-04T02:39:28Z-
dc.identifier.issn1674-9847-
dc.identifier.urihttp://hdl.handle.net/10397/89115-
dc.language.isoenen_US
dc.publisherKe Ai Publishing Communicationsen_US
dc.rights©2015, Institute of Seismology, China Earthquake Administration, etc. Production andhosting by Elsevier B.V. on behalf of KeAi Communications Co., Ltd. This is an open accessarticle under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).en_US
dc.rightsThe following publication Shen, Y., Chen, Q., & Xu, H. (2015). Monthly gravity field solution from GRACE range measurements using modified short arc approach. Geodesy and Geodynamics, 6(4), 261-266 is available at https://dx.doi.org/10.1016/j.geog.2015.05.009en_US
dc.subjectGravity field modelen_US
dc.subjectGravity recovery and climate experiment (Grace)en_US
dc.subjectGravity satelliteen_US
dc.subjectMass changeen_US
dc.subjectRange dataen_US
dc.subjectSatellite geodesyen_US
dc.subjectShort arc approachen_US
dc.subjectTime-Variable gravity fielden_US
dc.subjectTongji-Grace01en_US
dc.titleMonthly gravity field solution from GRACE range measurements using modified short arc approachen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage261-
dc.identifier.epage266-
dc.identifier.volume6-
dc.identifier.issue4-
dc.identifier.doi10.1016/j.geog.2015.05.009-
dcterms.abstractIn this paper we present a series of monthly gravity field solutions from Gravity Recovery and Climate Experiment (GRACE) range measurements using modified short arc approach, in which the ambiguity of range measurements is eliminated via differentiating two adjacent range measurements. The data used for developing our monthly gravity field model are same as Tongji-GRACE01 model except that the range measurements are used to replace the range rate measurements, and our model is truncated to degree and order 60, spanning Jan. 2004 to Dec. 2010 also same as Tongji-GRACE01 model. Based on the comparison results of the C2,0, C2,1, S2,1, and C15,15, S15,15, time series and the global mass change signals as well as the mass change time series in Amazon area of our model with those of Tongji-GRACE01 model, we can conclude that our monthly gravity field model is comparable with Tongji-GRACE01 monthly model.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationGeodesy and geodynamics, July 2015, v. 6, no. 4, p. 261-266-
dcterms.isPartOfGeodesy and geodynamics-
dcterms.issued2015-07-
dc.identifier.scopus2-s2.0-84959515342-
dc.identifier.eissn2589-0573-
dc.description.validate202101 bcrc-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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