supported by the National Natural Science Foundation of China (41174020, 41131067);the Fundamental Research Funds for the Central Universities (2014214020203);the open fund of Key Laboratory of Geospace Environment and Geodesy, Ministry of Education (14-02-011);the open fund of Guangxi Key Laboratory of Spatial Information and Geomatics (14-045-24-17)
Time-variable gravity data from the Gravity Recovery and Climate Experiment (GRACE) satellite mission are used to study terrestrial water storage (TWS) changes over the Pearl River Basin (PRB) for the period 200...
supported by the National 973Program of China(2013CB733302);the National Natural Science Foundation of China(41131067,41174020,41374023,41474019);the Open Research Fund Program of the State Key Laboratory of Geodesy and Earth's Dynamics(SKLGED2015-1-3-E);the open fund of State Key Laboratory of Geographic Information Engineering(SKLGIE2013-M-1-3);the open fund of Key Laboratory of Geospace Environment and Geodesy,Ministry of Education(13-02-05)
A new temporal gravity field model called WHU-Grace01s solely recovered from Gravity Recovery and Climate Experiment (GRACE) K-Band Range Rate (KBRR) data based on dynamic integral approach is presented in this pa...
supported by the National 973 Program of China(2013CB733302);the National Natural Science Foundation of China(41131067,41174020,41374023);the open fund of State Key Laboratory of Geographic Information Engineering(SKLGIE2013-M-1-3);the open fund of Key Laboratory of Geospace Environment and Geodesy,Ministry of Education(13-02-05);the Fundamental Research Funds for the Central Universities(2014214020203)
Qinghai-Tibet Plateau is the most complex region for crustal thickness inversion, while high-resolu- tion earth gravity model (EGM) makes it possible to obtain high precision gravity anomaly, which is a key pa- rame...