Efficient accuracy improvement of GRACE global gravitational field recovery using a new Inter-satellite Range Interpolation Method

被引:30
作者
Zheng, Wei [1 ,2 ]
Hsu, Houtse [1 ]
Zhong, Min [1 ]
Yun, Meijuan [3 ]
机构
[1] Chinese Acad Sci, Key Lab Dynam Geodesy, Inst Geodesy & Geophys, Wuhan 430077, Peoples R China
[2] Kyoto Univ, Disaster Prevent Res Inst, Uji, Kyoto 6110011, Japan
[3] Wuhan Univ Sci & Technol, Dept Appl Phys, Wuhan 430081, Peoples R China
基金
中国国家自然科学基金;
关键词
GRACE; WHIGG-GEGM01S model; Inter-satellite Range Interpolation Method; GPS/Levelling; Earth's gravitational field; TO-SATELLITE TRACKING; GRAVITY-FIELD; PERTURBATION-THEORY; MODEL; CHAMP; ACCELERATIONS; VALIDATION; HYDROLOGY; MISSION; ARCS;
D O I
10.1016/j.jog.2011.07.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
New studies on the influence of inter-satellite range on the accuracy of the Earth's gravitational field recovery were carried out based on the Inter-satellite Range Interpolation Method (IRIM). Firstly, the IRIM observation equation by introducing the precise inter-satellite range into the Line-Of-Sight (LOS) component of the relative orbital position vector was established for the first time using the original satellite observations including the orbital position of the spaceborne Global Positioning System (GPS) receiver, the inter-satellite range of the K-Band Ranging (KBR) system and the non-conservative force of the accelerometer (ACC). Secondly, the nine-point IRIM formula is shown by a comparison of multipoint IRIM formulas to be preferable for effectively improving the accuracy of the Earth's gravitational field recovery. Thirdly, the WHIGG-GEGM01S (GRACE Earth Gravity Model developed by Wuhan Institute of Geodesy and Geophysics) global gravity field model, complete up to degree and order 120, is produced using the GRACE Level-1B data products, acquired during 2008-01-01 to 2008-12-31 and released by the American Jet Propulsion laboratory (JPL). Cumulative geoid height and gravity anomaly errors are 1.098 x 10(-1) m and 1.741 x 10(-6) m/s(2) at degree 120, respectively. Finally, the availability of the WHIGG-GEGM01S model is validated by the GPS/Levelling observations in the U.S., Europe and Australia. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1 / 7
页数:7
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