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首页> 外文期刊>Annals Of Geophysics >A case study of detecting the triplet of 3S1 using superconducting gravimeter records with an alternative data preprocessing technique
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A case study of detecting the triplet of 3S1 using superconducting gravimeter records with an alternative data preprocessing technique

机译:使用超导重力仪记录和替代数据预处理技术检测3S1三联体的案例研究

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Due to their very low noise levels in the low frequency band (1 mHz), superconducting gravimeters (SGs) are particularly suitable to observe long-period free oscillations of the Earth. This case study is dedicated to the detection of the triplet of the seismic normal mode 3 S 1 that was excited by the December 26, 2004, Sumatra-Andaman earthquake (Mw = 9.3). Some SG records and the Hilbert-Huang transformation are used as an alternative data preprocessing technique, instead of the traditional detiding method. After removal of atmospheric pressure effects from the original SG records, we applied the Hilbert-Huang transformation to the SG residues, to select the signals that included the frequency band of interest, and to construct a new data series. Then, by applying the multi-station experimental technique to five 273-h-long common new data series recorded at different SG stations, we clearly observed all of the three singlets of the mode 3 S 1 , with the central singlet more evident compared to previous studies. Observations of the low-frequency modes 3 S 1 (n = 0, 1, 2, ...; l = = 1,2, ...) provide constraints on the inner and outer core structure. This case study provides an alternative data-preprocessing approach to observe the splitting frequencies of the low-frequency mode type 3 S 1 (n = 0, 1, 2, ...).
机译:由于超导重力仪(SGs)在低频频段(<1 mHz)中的噪声水平非常低,因此特别适合观察地球的长期自由振荡。本案例研究致力于检测2004年12月26日苏门答腊-安达曼地震(Mw = 9.3)激发的地震正常模式3 S 1的三重态。某些SG记录和Hilbert-Huang变换被用作替代的数据预处理技术,而不是传统的确定方法。从原始SG记录中去除大气压力影响后,我们将希尔伯特-黄(Hilbert-Huang)变换应用于SG残差,以选择包括感兴趣频段的信号,并构建一个新的数据序列。然后,通过将多站实验技术应用于在不同SG站记录的五个273小时长的常见新数据序列,我们清楚地观察到了模式3 S 1的所有三个单峰,与之前的学习。低频模式3 S 1(n = 0,1,2,...; l = = 1,2,...)的观察结果对内芯和外芯结构提供了约束。本案例研究提供了另一种数据预处理方法,用于观察3 S 1型低频模式(n = 0、1、2,...)的分裂频率。

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