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《Science of Surveying and Mapping》 2009-01
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Determination of gravity anomalies over China sea by combination of multi-satellite altimeter data

DENG Kai-liang①,BAO Jing-yang①,LIU Yan-chun①,ZHANG Chuan-yin②,XU Jun①(① Department of Hydrography and Cartography,Dalian Naval Academy,Dalian 116018,China;② Chinese Academy of Surveying and Mapping,Beijing 100039,China)  
Based on multi-satellite altimeter data(Geosat GM data,ERS-1 data,T/P data,new T/P data,ERS-2 data and GFO data),the direction-differential coefficient of geoid along track is computed using position information of altimetry point.Being combined with the azimuth angle of the direction of altimetry line,the deflection of the vertical is reckoned at the crossover point,and the 2'×2'gravity anomaly model of China sea and its adjacent sea areas(0o~41oN,105o~132oN) is obtained using inverse Vening-Meinesz formula.The gravity anomaly model is compared with CLS_SHOW9 model,the corresponding RMS of the difference is 8.15mgal,after eliminating error point where the difference is more than 20mgal(the proportion of the point eliminated is 3.3%),the corresponding RMS of the difference is 4.72mgal,and compared with the shi Pborne gravimetric date,the corresponding RMS of difference is 8.91mgal.
【Fund】: 实验室开放研究基金(1469990324233-04-03);; 测绘科技发展基金(214151926)
【CateGory Index】: P223.39
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