4.7 Article

Real-Time Earthquake Early Warning With Deep Learning: Application to the 2016 M 6.0 Central Apennines, Italy Earthquake

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 48, Issue 5, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020GL089394

Keywords

earthquake early warning; earthquake location; earthquake magnitude; machine learning; neural network; the 2016 Central Italy earthquake

Funding

  1. National Natural Science Foundation of China [41704040, 42004040]
  2. Open Fund from Engineering Research Center for Seismic Disaster Prevention and Engineering Geological Disaster Detection of Jiangxi Province [SDGD202009]
  3. National Science Foundation [EAR-1759810]
  4. Natural Science and Engineering Research Council of Canada Discovery Grant [RGPIN-2019-04297]
  5. Science foundation of East China University of Technology Grant [DHBK2019072]
  6. NERC [NE/R000794/1] Funding Source: UKRI

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The article introduces a novel deep learning Earthquake Early Warning (EEW) system that can determine earthquake locations and magnitudes with high reliability as early as 4 seconds after the earliest P phase, utilizing continuous seismic waveform streams.
Earthquake early warning (EEW) systems are required to report earthquake locations and magnitudes as quickly as possible before the damaging S wave arrival to mitigate seismic hazards. Deep learning techniques provide potential for extracting earthquake source information from full seismic waveforms instead of seismic phase picks. We developed a novel deep learning EEW system that utilizes fully convolutional networks to simultaneously detect earthquakes and estimate their source parameters from continuous seismic waveform streams. The system determines earthquake location and magnitude as soon as very few stations receive earthquake signals and evolutionarily improves the solutions by receiving continuous data. We apply the system to the 2016 M 6.0 Central Apennines, Italy Earthquake and its first-week aftershocks. Earthquake locations and magnitudes can be reliably determined as early as 4 s after the earliest P phase, with mean error ranges of 8.5-4.7 km and 0.33-0.27, respectively.

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