Recovery Water Storage Variation in China and Its Adjacent Area by Method of Point-Mass Model

被引:0
|
作者
Guo F. [1 ,2 ]
Miao Y. [3 ]
Xiao Y. [1 ,2 ]
Wang F. [3 ]
机构
[1] Xi'an Research Institute of Surveying and Mapping, Xi'an
[2] State Key Laboratory of Geo-Information Engineering, Xi'an
[3] Technical Division of Surveying and Mapping, Xi'an
来源
| 2017年 / Editorial Board of Medical Journal of Wuhan University卷 / 42期
关键词
GRACE time-variable gravity; Mass variation; Point-mass model; Regularization; Satellite gravimetry;
D O I
10.13203/j.whugis20150031
中图分类号
学科分类号
摘要
Method of point-mass model is investigated thoroughly. The ill-posed problem in parameter estimation is solved by Tikhonov regularization. Water storage variation in China and adjacent is recovered by method of point-mass model using GRACE time-variable gravity field data. The inversion result is verified by GLDAS hydrological model data and method of spheric harmonic coefficient. Meanwhile the water storage variation series of 4 characteristic points are calculated. The results show that because of the separated influence of different region mass anomaly on gravity field, the signal of water storage variation in local area which is recovered by method point-mass model is more powerful. By comparing the water storage variation series of 4 characteristic points, it is concluded that the correlation between the recovery results by method of point-mass model and GLDAS hydrological model data is stronger. © 2017, Research and Development Office of Wuhan University. All right reserved.
引用
收藏
页码:1002 / 1007
页数:5
相关论文
共 14 条
  • [1] Huang C., Hu X., Mass Redistribution to be Revealed by GRACE Project, Progress in Astronomy, 22, 1, pp. 35-45, (2004)
  • [2] Wahr J., Swenson S., Zlotnicki V., Et al., Time-variable Gravity from GRACE: First Result, Geophy Res Lett, 31, (2004)
  • [3] Wahr J., Molenaar M., Bryan F., Time Variability of the Earth's Gravity Field: Hydrological and Oceanic Effects and Their Possible Detection Using GRACE, J Geophys Res, 103, B12, pp. 30205-30229, (1998)
  • [4] Zhu G., Li J., Wen H., Investigation on the Mass Variation of Ice Sheet in Antarctic with GRACE Time-variable Gravity Models, Geomatics and Information Science of Wuhan University, 34, 10, pp. 1185-1190, (2009)
  • [5] Jiang M., Zhong M., Zhang Z., Et al., Influence of GIA on Ocean Mass Variations, Geomatics and Information Science of Wuhan University, 38, 38, pp. 1188-1191, (2013)
  • [6] Xing L., Li J., Li H., Et al., Detection of Co-seismic and Post-seismic Deformation Caused by the Sumatra-Adaman Earthquake Using GRACE, Geomatics and Information Science of Wuhan University, 34, 9, pp. 1080-1084, (2009)
  • [7] Zhai N., Wang Z., Wu Y., Et al., Recovery of Yangtze River Basin Water Storage by GRACE Observations, Geomatics and Information Science of Wuhan University, 34, 4, pp. 436-439, (2009)
  • [8] Forsberg R., Reeh N., Mass Change of the Greenland Ice Sheet from GRACE, The 1st International Symposium of IGFS, (2006)
  • [9] Baur O., Sneeuw N., Assessing Greenland Ice Mass Loss by Means of Point-mass Modeling: A Viable Methodology, J Geod, 85, pp. 607-615, (2011)
  • [10] Lu Z., Theory and Method of Earth Gravity Field, (1996)