Evaluation of Recent GRACE and GOCE Satellite Gravity Models and Combined Models Using GPS/Leveling and Gravity Data in China

被引:9
作者
Li, Jiancheng [1 ,2 ]
Jiang, Weiping [1 ,2 ,3 ]
Zou, Xiancai [1 ,2 ]
Xu, Xinyu [1 ,2 ]
Shen, Wenbin [1 ,2 ]
机构
[1] Wuhan Univ, Sch Geodesy & Geomat, Wuhan 430072, Peoples R China
[2] Minist Educ, Key Lab Geospace Environm & Geodesy, Wuhan, Peoples R China
[3] Wuhan Univ, GNSS Res Ctr, Wuhan 430072, Peoples R China
来源
GRAVITY, GEOID AND HEIGHT SYSTEMS | 2014年 / 141卷
关键词
GPS/leveling; Gravity anomaly; Geoid; Evaluation; Gravity field model;
D O I
10.1007/978-3-319-10837-7_9
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
A total of 649 GPS/Leveling points and 799897 2' x 2' gridded mean gravity anomalies in mainland China are used for the evaluation of the recently released Earth Gravitational Models (EGMs) including the GOCE only models (GO_CONS_GCF_2_TIM_R3 (GO_TIM_R3), GRACE only models ITG-Grace2010s, combined satellite gravity field models (GO_CONS_GCF_2_DIR_R3 (GO_DIR_R3), GOCO03S, DGM-1S, EIGEN-5S, EIGEN-6S), and combined gravity field models (EIGEN-51C, EIGEN-6C, GIF48, EGM2008) from satellite observations and ground gravity data sets. The statistical results show that in mainland China the most precise model is EIGEN-6C with the standard deviation (STD) +/-0.183 m of the quasi-geoid height differences compared with the GPS/Leveling data and the STD +/-22.5 mGal of the gravity anomaly differences compared with the gridded mean gravity anomalies from observations. For EGM2008, they are +/-0.240 m and +/-24.0 mGal respectively. Among the satellite only gravity models from GRACE, GOCE and LAGEOS observations, GO_TIM_R3 is the best one in mainland China, and the STDs of the corresponding quasi-geoid differences and the gravity anomaly differences are +/-0.459 m and +/-31.3 mGal respectively, which are nearly at the same levels as the ones for the models EIGEN-6S, GOCO03S and GO_DIR_R3. This shows that the GOCE mission can recover more medium-short wavelength gravity signals in mainland China than former satellite gravity missions.
引用
收藏
页码:67 / 74
页数:8
相关论文
共 9 条
[1]  
ESA, 2011, GOCE NEWSLETTER DEC
[2]   The static gravity field model DGM-1S from GRACE and GOCE data: computation, validation and an analysis of GOCE mission's added value [J].
Farahani, H. Hashemi ;
Ditmar, P. ;
Klees, R. ;
Liu, X. ;
Zhao, Q. ;
Guo, J. .
JOURNAL OF GEODESY, 2013, 87 (09) :843-867
[3]  
Forste C, 2011, GEOPH RES EGU GEN AS, V13
[4]  
[李建成 Li Jiancheng], 2012, [测绘学报, Acta Geodetica et Cartographica Sinica], V41, P651
[5]  
Mayer-Gurr T, 2012, GGHS 2012 VEN OCT 20
[6]  
Mayer-Gurr T., 2010, ITG-Grace2010 Gravity Field Model
[7]   First GOCE gravity field models derived by three different approaches [J].
Pail, Roland ;
Bruinsma, Sean ;
Migliaccio, Federica ;
Foerste, Christoph ;
Goiginger, Helmut ;
Schuh, Wolf-Dieter ;
Hoeck, Eduard ;
Reguzzoni, Mirko ;
Brockmann, Jan Martin ;
Abrikosov, Oleg ;
Veicherts, Martin ;
Fecher, Thomas ;
Mayrhofer, Reinhard ;
Krasbutter, Ina ;
Sanso, Fernando ;
Tscherning, Carl Christian .
JOURNAL OF GEODESY, 2011, 85 (11) :819-843
[8]   The development and evaluation of the Earth Gravitational Model 2008 (EGM2008) [J].
Pavlis, Nikolaos K. ;
Holmes, Simon A. ;
Kenyon, Steve C. ;
Factor, John K. .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2012, 117
[9]  
[No title captured]