Abstract
Deep learning has emerged as a transformative tool for enhancing the extraction of reliable information from seismograms, addressing the increasing demand for precise and efficient seismic data analysis. We introduce an innovative encoder–decoder deep learning model, named WaveDenoiser, designed for noise reduction in the time domain, thereby eliminating the need for spectrogram computations that have been used for existing deep learning tools and significantly improving processing speed. Utilizing the benchmark data-set that is Stanford Earthquake Dataset, we developed three models of varying sizes: base, medium, and large. Notably, the large (referred to as WaveDenoiser) model demonstrated superior performance, achieving a median signal-to-noise ratio improvement of 8.8 dB on in-distribution unseen data (in the same geographic region) and 7.7 dB on out-distribution unseen data (in a new geographic region), outpacing both the base and medium models. Further evaluation of the WaveDenoiser model revealed a reduction in median arrival-time errors by 0.02 s for P waves and 0.01 s for S waves when processing waveforms prior to phase picking using PhaseNet on in-distribution unseen data. When tested on out-distribution unseen data, the model also effectively reduced the P-wave median arrival-time error by 0.02 and 0.01 s in median arrival-time error for S waves. Importantly, the application of WaveDenoiser resulted in a significant reduction of phase picking outliers by 1.1% to 3.6% for both P and S waves. In addition, we achieved over five times acceleration in processing speed compared with the seisBench implementation of DeepDenoiser. Our findings underscore the potential of WaveDenoiser as a powerful tool for improving seismic data analysis and processing efficiency.
| Original language | English |
|---|---|
| Pages (from-to) | 192-204 |
| Number of pages | 13 |
| Journal | Bulletin of the Seismological Society of America |
| Volume | 116 |
| Issue number | 1 |
| DOIs | |
| State | Published - Feb 2026 |
Funding
The authors would like to acknowledge the U.S. Department of Energy (DOE), National Nuclear Security Administration’s Office of Defense Nuclear Nonproliferation Research and Development, for supporting this work. This work has been authored in part by UT-Battelle, LLC, under Contract DE-AC05-00OR22725 with the U.S. DOE. The U.S. Government retains, and the publisher, by accepting the article for publication, acknowledges that the U.S. Government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this article, or allow others to do so, for U.S. Government purposes. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. This research used resources of the Compute and Data Environment for Science (CADES) and Oak Ridge Leadership Computing Facility at Oak Ridge National Laboratory (ORNL), which is supported by the DOE Office of Science under Contract Number DE-AC05-00OR22725. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan (http://energy.gov/ downloads/doe-public-access-plan, last accessed April 2025). The authors thank Jason Hite for his contributions to an early version of the source code. The authors acknowledge helpful suggestions from Monica Maceira, Erin Cunningham, and Karl Pazdernik. The authors appreciate the support of Stefano Parolai for cross-checking the results of the S-transform denoised waveform in Figure S21. The authors thank Editor-in-Chief Martin Mai, Associate Editor Stefano Parolai, and two anonymous reviewers for their constructive comments that significantly improved the article.
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