GOBEYONDGOBEYOND

  • The project
    • Project Overview
    • Our Vision
    • Who We Are
    • Advisory Board
  • Co-creation
    • Living Labs
    • Pilot Sites
    • Community of Practice
  • Tools
    • Platforms
    • Innovation Prize Recap
  • Docs
    • Publications
    • Deliverables
  • News & Events
    • News
    • Events
      • 1st Workshop Recap
  • Media
    • Communication Kit
    • Videos
    • Newsletters
    • Press Releases
  • Contact
Subscribe to our Newsletter
admin
admin
Wednesday, 18 December 2024 / Published in New publications, News

Publication: Groundbreaking Research Unveils New Earthquake Early Warning System Using Initial Seismic Signals

New research reveals that the initial signals emitted during an earthquake can effectively track the evolution of fault rupture in real-time, offering the potential to alert populations before destructive seismic waves arrive. This study, conducted by Raffaele Rea, Simona Colombelli, Luca Elia, and Aldo Zollo from the Department of Physics at the University of Naples Federico II, was recently published in Nature Communications Earth & Environment.

During an earthquake, seismic waves originate deep underground, propagating through the Earth and reaching the surface within seconds, causing severe damage to people, buildings, and infrastructure. Although earthquake prediction remains elusive, predicting the impact of these events and sending warnings to specific areas before the arrival of destructive waves is possible through Earthquake Early Warning (EEW) systems.

In their recent paper, the team demonstrates the effectiveness of their advanced EEW system, applied to the magnitude 7.8 earthquake that struck the Turkey-Syria border region in February 2023. Their approach uses a sophisticated ground-motion prediction method based on the detection of primary (P) waves, which allows for the real-time identification of areas where ground shaking is likely to exceed predefined thresholds.

The system’s performance was validated through a retrospective analysis of hundreds of accelerometer readings near the earthquake’s source. Remarkably, an alert was generated approximately 10 seconds after the earthquake’s origin, with a 95% success rate in notifying sites within the affected zone, providing lead times of 10 to 60 seconds in high-risk areas. The study shows that the anticipated strong shaking region could be reliably identified approximately 20 seconds after the rupture initiation.

As time progresses, the system precisely outlines the seismic rupture’s development, highlighting its bilateral propagation in the northeast-southwest direction, as inferred from kinematic source models.

These findings indicate that P-wave-based EEW systems can deliver timely and accurate alerts, significantly reducing potential damage and enhancing safety in earthquake-prone regions.

You can read the article at https://www.nature.com/articles/s43247-024-01507-3

Snapshots of the P-wave based shake map of the Mw 7.8, February 6, 2023 Turkey–Syria where you can see the earthquake computed at 8.9 s after the event origin time (OT).
  • Tweet

What you can read next

1st GOBEYOND Workshop
GOBEYOND’s First Living Lab in Attica: A Step Towards Enhanced Civil Protection
Wildfires in Attica: Managing a Multi-Risk Challenge in the Age of Climate Crisis

Leave a Reply

Your email address will not be published. Required fields are marked *

This project has received funding from the European Union’s Horizon Europe programme for research and innovation under grant agreement No. 101121135.

Stay Connected!

Subscribe to our Newsletter!

© 2024. All rights reserved.

TOP