The construction of power spectral density function and its application to the computation of gravity functions
CHEN Xin1,2, DENG Kai-Liang2, ZHAI Guo-Jun2, BAO Jing-Yang1, OUYANG Yong-Zhong2, LU Xiu-Ping2, WU Tai-Qi2
1. Department of Hydrography and Cartography, Dalian Naval Academy, Dalian 116018, China;
2. Naval Institute of Hydrographic Surveying and Charting, Tianjin 300061, China
The formula of the relation between gravity anomaly system error and geoid was inferred based on the Stokes formula. To verify the reliability of this relation, the authors designed the simulation experiment based on the EGM2008 gravity model and calculated the propagation of gravity anomaly system error. Using error formula to estimate the accuracy of Stokes geoid will be influenced by the error edge effect. The relation between integral radius and estimated accuracy of the formula is given on the basis of the simulation experiment.
陈欣, 邓凯亮, 翟国君, 暴景阳, 欧阳永忠, 陆秀平, 吴太旗. Stokes积分中重力异常系统差对大地水准面影响的仿真研究[J]. 物探与化探, 2015, 39(S1): 72-75.
CHEN Xin, DENG Kai-Liang, ZHAI Guo-Jun, BAO Jing-Yang, OUYANG Yong-Zhong, LU Xiu-Ping, WU Tai-Qi. The construction of power spectral density function and its application to the computation of gravity functions. Geophysical and Geochemical Exploration, 2015, 39(S1): 72-75.