Multivariate variational mode decomposition to extract the stripe noise in GRACE harmonic coefficients

被引:0
|
作者
Jian, Guangyu [1 ]
Zou, Fang [1 ]
Xu, Chuang [1 ,2 ,3 ]
Yan, Zhengwen [4 ]
机构
[1] Guangdong Univ Technol, Sch Civil & Transportat Engn, Dept Geodesy & Geomat Engn, Guangzhou 510006, Peoples R China
[2] Huazhong Univ Sci & Technol, Natl Precise Grav Measurement Facil, Wuhan 430074, Peoples R China
[3] Guangdong Univ Technol, Cross Res Inst Ocean Engn Safety & Sustainable Dev, Guangzhou 510006, Peoples R China
[4] Southern Univ Sci & Technol, Dept Earth & Space Sci, Shenzhen 518055, Peoples R China
基金
中国国家自然科学基金;
关键词
Satellite geodesy; Satellite gravity; Time variable gravity; Spatial analysis; GRAVITY-FIELD; ERRORS; VARIABILITY;
D O I
10.1093/gji/ggae241
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
In this work, a novel method has been developed to remove the north-south stripe noise in the Level-2 spherical harmonic coefficient products collected by the Gravity Recovery and Climate Experiment (GRACE) mission. The proposed method extracts the stripe noise from the equivalent water height (EWH) map via the Multivariate Variational Mode Decomposition algorithm. The idea behind our method is to extract the cofrequency mode in multiple-channel series in the longitude direction. The parameters of our method are empirically determined. The investigation in a closed-loop simulation proves the improvement of our methods compared with the Singular Spectrum Analysis Spatial (SSAS) filter. Subsequently, the spatial-domain and spectral-domain investigations are conducted by using real GRACE data. Our method only suppresses stripe noise at low latitudes (30 degrees S-30 degrees N) and imposes an order-dependent impact on spherical harmonic coefficients but with potential oversmoothing. Meanwhile, the well-documented water level proves that our method further reduces outliers in a time-series of localized mass variations compared with the SSAS filter. More importantly, users are allowed to reduce the filtering strength of our method to preserve small-scale strong signals while suppressing stripe noise. Moreover, noise levels over the ocean at low latitudes are evaluated as well. The noise level of our method using empirical parameters is 32.48 mm of EWH, with 31.54 and 53.52 mm for DDK6 and SSAS, respectively. Our work introduces a novel method to address the issue of north-south stripe noise in the spatial domain.
引用
收藏
页码:1742 / 1754
页数:13
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