Acta Geodaetica et Cartographica Sinica ›› 2017, Vol. 46 ›› Issue (7): 815-823.doi: 10.11947/j.AGCS.2017.20160643

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Evaluation of the Geopotential Value for the Local Vertical Datum of China Using GRACE/GOCE GGMs and GPS/Leveling Data

HE Lin1,3, LI Jiancheng1,2, CHU Yonghai1,2   

  1. 1. School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China;
    2. Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan 430079, China;
    3. Guangxi Key Laboratory of Spatial Information and Geomatics, Guilin University of Technology, Guilin 541006, China
  • Received:2016-12-16 Revised:2017-06-20 Online:2017-07-20 Published:2017-07-25
  • Supported by:
    National Key Research and Development Plan (No. 2016YFB0501702);The National Key Basic Research and Development Program of China (973 Program) (No. 2013CB733301);The Open Fund of Guangxi Key Laboratory of Spatial Information and Geomatics (No. 16-380-25-33)

Abstract: The main purpose of this paper is to estimate the zero height geopotential value for the China Local Vertical Datum. The method used is based on a gravimetric approach and benefits from the significant improvements in the determination of the global gravity field by the recent satellite gravity missions such as GRACE and GOCE. The performance of GOCE-based or GRACE/GOCE-based Global Geopotential Models (GGMs) is assessed for estimation of geopotential of the regional vertical datum of China using the GPS/Levelling BMs (benchmarks) from vertical control network. We should conver the normal height to orthometric height. From the evaluation with the GPS/Levelling BMs, it is concluded that the GOCE-based or GRACE/GOCE-based GGMs provide an absolute accuracy at of 40 cm, up to their maximum degree and order. Factors that affect the geopotential value of vertical datum include the GOCE commission and omission errors. Among these factors, the effect of the GOCE omission error is investigated by extending the models with the high resolution gravity field model EGM2008. When extending the GOCE-based or GRACE/GOCE-based models with the high resolution gravity field model EGM2008, we should provide the same parameters. At the same time we should unify the frame and tide system between the GGMs and GPS/Levelling dataset. The result shows that, the effect of the GOCE omission error is at the level of 1.6 m2s-2 (about 16 cm), in China, is at decimetre-level when computing local vertical datum geopotential, the effect of the tide system is about 4-6 cm. The vertical datum geopotential of China is estimated as 62 636 852.704 5 m2s-2.

Key words: GRACE, GOCE, satellite gravity, vertical datum, omission error, tide system

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