测绘学报

• 学术论文 •    

GRACE时变重力位系数误差的改进去相关算法

詹金刚1,王勇2,郝晓光2   

  1. 1. 中科院测量与地球物理研究所
    2. 中国科学院测量与地球物理研究所
  • 收稿日期:2010-04-15 修回日期:2010-10-27 出版日期:2011-08-25 发布日期:2011-08-25
  • 通讯作者: 王勇

Improved Method for Removal of Correlated Errors in GRACE Data

  • Received:2010-04-15 Revised:2010-10-27 Online:2011-08-25 Published:2011-08-25

摘要: Gravity Recovery and Climate Experiment(GRACE)卫星时变重力场模型的高阶位系数存在较大误差,用它反演的重力场结果中表现为严重的条带噪声。SWENSON提出的滑动窗多项式拟合去相关误差方法在赤道两侧区域取得了显著效果,但其在文献中并没有说明实现的具体步骤,因而许多学者在利用其思想进行滤波时并没有达到其文献中的滤波效果。本文针对滑动窗的特点,提出了滑动窗去相关误差的改进方法。改进的滑动窗去相关误差方法应用于GRACE时变重力场模型时,在赤道两侧区域取得了显著的去条带误差效果,并利用全球地面资料同化系统GLDAS土壤湿度资料验证了该方法的正确性。

Abstract: The error of the GRACE potential coefficients increases towards higher spherical-harmonic degrees, and the result of gravity anomalies computed from GRACE data will be dominated by errors such as stripes. Swenson proposed an empirical moving window filtering method to remove the correlation and shows a significant effect in the region on both sides of the equator, but it is not provided more details about the method in the paper. Many people did not get the desired effect followed the principle of Swenson when filtering. In this paper, we improved the technology of data processing and achieved the expected results. More, we calculated the global gravity change trends using GRACE data based on this method. The results can more clearly and reasonably reflect the location of gravity change and prove that the improved method is more reasonable and effective in producing GRACE data