CEEMD-UNet融合的低信噪比高频GNSS同震位移信号增强方法

A CEEMD-UNet Fusion-Based Signal Enhancement Method for Low-SNR High-Rate GNSS Coseismic Displacements

  • 摘要: 高频全球导航卫星系统(global navigation satellite system,GNSS)技术可直接获取地表同震位移,是地震监测的核心手段之一。针对中小地震或远震中距场景下高频GNSS同震位移观测数据信噪比偏低、传统降噪方法难以兼顾噪声抑制与信号特征保留的问题,提出了一种完备总体经验模态分解(complementary ensemble empirical mode decomposition,CEEMD)与UNet网络(CEEMD-UNet)融合的降噪方法。首先,通过CEEMD自适应分解非平稳同震位移,有效克服了传统降噪方法的局限性;然后,利用UNet网络对分解得到的本征模态函数(intrinsic mode function,IMF)进行精准去噪,实现了噪声高效抑制与同震信号特征保留的平衡。合成数据测试结果表明,去噪后E、N和U方向的平均互相关系数均优于0.85,平均信噪比分别提升14.72、12.84和38.77倍;基于2018年美国阿拉斯加安克雷奇MW7.0地震的GNSS实际观测数据验证,去噪后各台站在E、N、U方向的平均标准差分别降低了41.39%、48.79%和67.90%,平均信噪比分别提升了5.05倍、2.89倍和0.96倍。与CEEMD-WD和UNet降噪方法相比,提出的CEEMD-UNet方法在波形一致性、振幅保持性及跨场景适应性上优势显著,可为低信噪比高频GNSS地震数据处理提供技术支撑。

     

    Abstract: Objectives: High-rate global navigation satellite system (GNSS) technology enables the direct acquisition of surface coseismic displacements and serves as a vital tool in the field of earthquake monitoring. However, in scenarios involving moderate-to-small earthquakes or distant epicentral distances, the signal-tonoise ratio (SNR) of recorded data is typically low, which severely restricts the accuracy of subsequent studies such as source parameter inversion. Methods: To address this, a novel denoising method fusing complementary ensemble empirical mode decomposition (CEEMD) with a UNet network (CEEMD-UNet) is proposed. This method first adaptively decomposes non-stationary coseismic displacements through CEEMD, effectively overcoming the limitations of traditional denoising methods; then, the UNet network is utilized to precisely denoise the decomposed intrinsic mode functions (IMFs), achieving a balance between efficient noise suppression and the preservation of coseismic signal characteristics. Results: Tests on synthetic data demonstrate that the average cross-correlation coefficient (CC) between the denoised signals and the true signals in the east (E), north (N), and up (U) components exceeds 0.85, with the average SNR improved by factors of 14.72, 12.84, and 38.77, respectively. Further validation based on actual GNSS observation data from the 2018 Anchorage, Alaska, MW7.0 earthquake shows that the average standard deviation (STD) in the E, N, and U components across all stations after denoising were reduced by 41.39%, 48.79%, and 67.90% respectively, and the SNR were improved by factors of 5.05, 2.89, and 0.96, respectively. Most importantly, compared with the CEEMD-Wavelet denoising (CEEMD-WD) method and UNet denoising method, the CEEMD-UNet method exhibits significant advantages in terms of waveform consistency, amplitude preservation characteristics, and cross-scenario robustness. It can provide technical support for the processing of low SNR high-rate GNSS seismic data. Conclusions: The effectiveness of hybrid signal processing strategies in geophysical data cleaning should be confirmed. The proposed CEEMD-UNet framework provides a reliable solution for improving the quality of high-rate GNSS data and holds significant value for high-precision applications such as earthquake early warning and source mechanism inversion.

     

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