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GRACE卫星关键载荷实测数据的有效处理和地球重力场的精确解算
引用本文:郑伟,许厚泽,钟敏,员美娟,周旭华,彭碧波.GRACE卫星关键载荷实测数据的有效处理和地球重力场的精确解算[J].地球物理学报,2009,52(8):1966-1975.
作者姓名:郑伟  许厚泽  钟敏  员美娟  周旭华  彭碧波
作者单位:1.中国科学院测量与地球物理研究所动力大地测量学重点实验室, 武汉 430077;2.日本京都大学防灾研究所,京都 611-0011;3.武汉科技大学应用物理系,武汉 430081
基金项目:国家自然科学基金,中国科学院知识创新工程重要方向项目,国家高技术研究发展计划(863),日本JSPS基盘研究项目 
摘    要:首先对美国喷气推进实验室(JPL)公布的2007-06-01~2007-12-31时间段内的GRACE Level 1B卫星GPS轨道位置和速度、K波段系统星间速度、加速度计非保守力以及恒星敏感器姿态实测数据对应进行了轨道拼接、粗差探测、线性内插、重新标定、坐标转换、误差分析等有效处理;其次,基于改进的能量守恒法恢复了120阶GRACE地球重力场,在120阶处累计大地水准面精度为25.313 cm;最后,检验了本文地球重力场模型IGG-GRACE的可靠性,同时分析了IGG-GRACE解算精度在低频部分略优于德国波兹坦地学研究中心(GFZ)公布的EIGEN-GRACE02S地球重力场模型,而在中高频部分略低的原因.

关 键 词:GRACE  关键载荷  实测数据  能量守恒法  地球重力场  
收稿时间:2008-12-16
修稿时间:2009-6-4

Effective processing of measured data from GRACE key payloads and accurate determination of Earth's gravitational field
ZHENG Wei,HSU Houtse,ZHONG Min,YUN Mei-Juan,ZHOU Xu-Hua,PENG Bi-Bo.Effective processing of measured data from GRACE key payloads and accurate determination of Earth''s gravitational field[J].Chinese Journal of Geophysics,2009,52(8):1966-1975.
Authors:ZHENG Wei  HSU Houtse  ZHONG Min  YUN Mei-Juan  ZHOU Xu-Hua  PENG Bi-Bo
Institution:1.Key Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China;2.Disaster Prevention Research Institute, Kyoto University, Uji, Kyoto 611-0011, Japan;3.Department of Applied Physics, Wuhan University of Science and Technology, Wuhan 430081, China
Abstract:Firstly, the GRACE Level 1B measured data including the orbital position and velocity of GPS receiver, intersatellite range rate of K-band ranging system, nonconservative force of accelerometer and attitude of star camera assembly between 2007-06-01~2007-12-31 provided by the American Jet Propulsion Laboratory (JPL) are processed effectively by orbital connection, gross error detection, linear interpolation, recalibration, coordinate transformation, error analysis, and so on. Secondly, the GRACE Earth′s gravitational field complete up to degree and order 120 is recovered based on the improved energy conservation principle, the cumulative geoid height error is 25.313 cm at degree 120. Finally, the dependability of the Earth′s gravitational field model IGG-GRACE is verified in the paper, and the reasons why the accuracy of IGG-GRACE is a little superior to the Earth′s gravitational field model EIGEN-GRACE02S provided by the German GeoForschungsZentrum Potsdam (GFZ) in the low frequency range and is slightly lower than that in the medium-high frequency band are analyzed.
Keywords:GRACE
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