Acta Geodaetica et Cartographica Sinica ›› 2017, Vol. 46 ›› Issue (9): 1088-1097.doi: 10.11947/j.AGCS.2017.20170101

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Recovery of the Earth's Gravity Field Based on Spaceborne Atom-interferometry and Its Accuracy Estimation

ZHU Zhu1, ZHAO Yanbin1, LIAO He1, TU Haibo2, ZHANG Guowan3, WEI Xiaogang3   

  1. 1. Shanghai Institute of Satellite Engineering, Shanghai 201109, China;
    2. State Key Laboratory of Geodesy and Earth's Geodynamics, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China;
    3. Quantum Engineering Research Center, China Aerospace Science and Technology Corporation, Beijing 100854, China
  • Received:2017-03-02 Revised:2017-07-28 Online:2017-09-20 Published:2017-10-12
  • Supported by:
    The National Natural Science Foundation of China(Nos. 41504034;11574099)

Abstract: The electrostatic gravity gradiometer has been successfully applied as a core sensor in satellite gravity gradiometric mission GOCE, and its observations are used to recover the Earth's static gravity field with a degree and order above 200. The lifetime of GOCE has been over, and the next generation satellite gravity gradiometry with higher resolution is urgently required in order to recover the global steady-state gravity field with a degree and order of 200~360. High potential precision can be obtained in space by atom-interferometry gravity gradiometer due to its long interference time, and thus the atom-interferometry-based satellite gravity gradiometry has been proposed as one of the candidate techniques for the next satellite gravity gradiometric mission. In order to achieve the science goal for high resolution gravity field measurement in the future, a feasible scheme of atom-interferometry gravity gradiometry in micro-gravity environment is given in this paper, and the gravity gradient measurement can be achieved with a noise of 0.85mE/Hz1/2. Comparison and estimation of the Earth's gravity field recovery precision for different types of satellite gravity gradiometry is discussed, and the results show that the satellite gravity gradiometry based on atom-interferometry is expected to provide the global gravity field model with an improved accuracy of 7~8cm in terms of geoid height and 3×10-5 m/s2 in terms of gravity anomaly respectively at a degree and order of 252~290.

Key words: Earth's gravity field, satellite gravity gradiometry, space-borne gravity gradiometer, atom-interferometry

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