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引用本文:梁子亮,陈路,解琨,岳建平,吉渊明.?????????????????????????????????????[J].大地测量与地球动力学,2015,35(1):40-44.
作者姓名:梁子亮  陈路  解琨  岳建平  吉渊明
作者单位:1 江苏省基础地理信息中心, 南京市北京西路75号, 210013
2 河海大学地球科学与工程学院, 南京市西康路1号, 210098
3 浙江省测绘科学技术研究院, 杭州市保俶北路83号, 310012
摘    要:??????????????????о????????????????????????????????????????????????????????????????С????????????????????????????????????????????????????ξ????????η??????????????????????FFT?????????????????????????????????????????????????????????????????????????????????????????????????????????????????б??????????????±5.231 58 mGal???????????????????EGM96??EGM2008???????????б?????????????????±0.694 57 m??±0.029 51 m??

关 键 词:??????    ???????    ??????    ??????????  FFT  
收稿时间:2013-10-12

Inversion of Marine Gravity Anomalies and Geoid Using Multi-Satellite Altimeter Data
LIANG Ziliang,CHEN Lu,XIE Kun,YUE Jianping,JI Yuanming.Inversion of Marine Gravity Anomalies and Geoid Using Multi-Satellite Altimeter Data[J].Journal of Geodesy and Geodynamics,2015,35(1):40-44.
Authors:LIANG Ziliang  CHEN Lu  XIE Kun  YUE Jianping  JI Yuanming
Institution:1 Provincial Geomatics Centre of Jiangsu, 75 West-Beijing Road, Nanjing 210013, China
2 School of Earth Sciences and Engineering,Hohai University,1 Xikang Road, Nanjing 210098, China
3 Zhejiang Academy of Surveying and Mapping,83 North-Baoshu Road, Hangzhou 310012, China
Abstract:Multi-satellite altimeter data were used to study and the method of combined crossover adjustment was completed.Systematic bias might be reduced with the method.The meridional component and prime vertical component of the residual vertical deflections of Zhejiang offshore were determined using the weighted method of along track least squares with an appropriate search radius.On the basis of remove restore method and FFT technology,the gravity anomaly model and geoid model gridded with a spatial resolution of 2.5′ of Zhejiang offshore were determined using the residual vertical deflections with an appropriate integration radius,under the consideration of effects of innermost zone.The gravity anomaly computed by the method was compared with the shipborne gravity,the RMS of the difference is ±5.231 58 mGal.The marine geoid was compared with the  results calculated with  EGM96 and EGM2008,the RMS of the difference is ±0.694 57 m and ±0.029 51 m.
Keywords:satellite altimetry  deflection of the vertical  gravity anomaly  marine geoid  FFT
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