Calculation of geoid undulations and gravity anomalies in the South China sea by using the TOPEX/Poseidon and Geosat altimeter data
Zhang, Youguang1,2; Zhang, Jie2,3; Ji, Yonggang2; Zhang, Huiqin4
2003
会议日期10 24, 2002 - 10 26, 2002
会议地点Hangzhou, China
卷号4892
期号4892
DOI10.1117/12.466798
页码521-528
英文摘要In this paper, using TOPEX/Poseidon (9-346cycle) and Geosat/ERM(l-60cycle) altimeter data, the author applies combined adjustment model for calculating the South China Sea geoid undulations after data preprocessing. The difference between calculation result and OSU91A model is 30cm (spatial resolution is 22km). In addition, 12′ × 12′ South China Sea gravity anomalies are calculated by using above geoid data and improved Stokes inverse formula. Contrasted with Scripps Institution of Oceanography gravity anomalies data, the accuracy of computation of gravity anomalies is 12 × 10-5 m/s2. These computations show that calculation speed is fast and calculation efficiency is high, so the method can calculate rapidly gravity anomalies in special sea area.
会议录Proceedings of SPIE - The International Society for Optical Engineering
会议录出版者SPIE
语种英语
ISSN号0277786X
内容类型会议论文
源URL[http://ir.fio.com.cn:8080/handle/2SI8HI0U/7125]  
专题业务部门_海洋物理与遥感研究室
作者单位1.Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266061, China;
2.First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;
3.Key Lab. Marine Sci./Numer. Modeling, State Oceanic Administration, Qingdao 266061, China;
4.Department of Mathematics, NeiMongol University, Hohhot 010021, China
推荐引用方式
GB/T 7714
Zhang, Youguang,Zhang, Jie,Ji, Yonggang,et al. Calculation of geoid undulations and gravity anomalies in the South China sea by using the TOPEX/Poseidon and Geosat altimeter data[C]. 见:. Hangzhou, China. 10 24, 2002 - 10 26, 2002.
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