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A Novel Time-Frequency Similarity Method for P-Wave First-Motion Polarity Detection
Yanji Yao1,2, Xin Xu3, Jing Wang1
1School of Water Conservancy, Yunnan Agricultural University, Kunming 650201, China.
Sensors (Basel, Switzerland)
|July 12, 2025
Summary
A new time-frequency similarity coefficient (TFSC) method improves P-wave polarity detection in noisy seismic data. This noise-resistant approach enhances earthquake analysis accuracy without preprocessing.
Area of Science:
- Seismology
- Earthquake Science
- Signal Processing
Background:
- P-wave first-motion polarity is crucial for earthquake focal mechanism determination.
- Seismic noise complicates accurate detection of P-wave onsets and polarities.
- Existing methods like normalized cross-correlation (NCC) are sensitive to noise.
Purpose of the Study:
- To develop a noise-resistant method for detecting P-wave first-motion polarity.
- To improve the accuracy of earthquake location and focal mechanism inversion.
Main Methods:
- Proposed a novel time-frequency similarity coefficient (TFSC) method based on the normal time-frequency transform (NTFT).
- Calculated relative delays and similarity coefficients using the real part of NTFT coefficients.
- Validated the TFSC method using synthetic and real earthquake data.
Main Results:
- The TFSC method demonstrated superior robustness and reliability compared to conventional NCC.
- Effective detection of P-wave polarity was achieved even without filtering or preprocessing.
- The method accurately identified relative delays and similarity coefficients.
Conclusions:
- The TFSC method offers a significant advancement for accurate P-wave polarity detection in noisy seismic environments.
- This technique shows strong potential for practical applications in seismology.
- Provides a novel perspective for seismic signal analysis.
Keywords:
P-wave first-motion polaritynormal time–frequency transformseismic noisetime–frequency similarity coefficient
