Acta Geodaetica et Cartographica Sinica ›› 2022, Vol. 51 ›› Issue (11): 2245-2254.doi: 10.11947/j.AGCS.2022.20210222

• Geodesy and Navigation •     Next Articles

A two-step integral method for geoid determination using generalized band-limited airborne vector gravity data

HUANG Motao1,2, DENG Kailiang1, WU Taiqi1, WANG Weiping2,3, OUYANG Yongzhong2, CHEN Xin1, WANG Xu1   

  1. 1. Naval Research Institute, Tianjin 300061, China;
    2. Key Laboratory of Marine Environmental Survey Technology and Application, Ministry of Natural Resources, Guangzhou 510300, China;
    3. South China Sea Marine Survey and Technology Center, State Oceanic Administration, Guangzhou 510300, China
  • Received:2021-05-25 Revised:2021-10-18 Published:2022-11-30
  • Supported by:
    The National Natural Science Foundation of China(Nos. 42274015;41804011;42174013;41706111;41774021);The National Key Research and Development Program of China(Nos. 2016YFB0501704;2016YFC0303007);The PLA Basic Research Program of China(173 Program)(No. 2019-JCJQ-ZD-017)

Abstract: According to the generalized band-limited horizon boundary value theory of physical geodesy survey, a two-step integral method is proposed to determine the geoid based on the horizontal component of band-limited airborne vector gravity data. Firstly,based on the solution of generalized band-limited horizon boundary value problem, we transform the horizontal component of band-limited airborne vector gravity data into a band-limited disturbing gravity potential at flight level. Secondly, the band-limited disturbing gravity potential is continued downward to the sea level by using the solution of the band-limited Dirichlet boundary value problem. Finally, according to the Bruns formula, the band-limited disturbing gravity potential at sea level is converted to the geoid. Simulation experiments using EGM2008 gravity field model show that the solution of generalized band-limited horizontal boundary value problem has a good low-pass filtering characteristic, which can weaken the effect of high-frequency noises in the observed value. The accuracy of the band-limited geoid obtained by the solution to the band-limited Dirichlet boundary problem is better than 3 cm when the error of the horizontal component of band-limited airborne vector gravity data is taken as 3 mGal and the flying height as 6 km. It indicates that the two-step integral method has good stability and effectiveness.

Key words: horizontal component of band-limited airborne vector gravity data, geoid, two-step integral method, generalized band-limited horizon boundary value problem, band-limited Dirichlet boundary value problem

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