ShakeAlert Earthquake Early Warning System Performance During the Mw 7.0 Offshore Cape Mendocino Earthquake

ABSTRACT The 5 December 2024 Mw 7.0 Offshore Cape Mendocino earthquake was a challenging test of the U.S. West Coast ShakeAlert earthquake early warning system due to its offshore epicenter and limited near-source station coverage. We analyzed real-time performance of all components of the ShakeAlert system, including the seismic algorithms (earthquake point-source integrated code [EPIC] and Finite-fault rupture Detector [FinDer]), the geodetic algorithm (Geodetic First Approximation of Size and Time–peak ground displacement [GFAST-PGD]), and network telemetry during the event. EPIC created the first solution for this earthquake 15 s after origin time with an initial magnitude estimate of M 5.6 and location error of 10 km from the Advanced National Seismic System epicenter. An early spurious trigger from station CE.89101 fortuitously maintained location accuracy and, correspondingly, magnitude accuracy. FinDer contributed its first solution at 18 s with a location estimate closer to the seismic network and produced two distinct rupture geometries, leading to minor fluctuations in estimated intensity contours. GFAST-PGD did not meet alerting thresholds but otherwise performed as expected. Network latencies were <2 s for most stations, supporting the rapid detection of this earthquake by the system. Roughly five million alerts were delivered to cell phone devices in California and Oregon during this event. This was also the first instance of a school district-wide ShakeAlert-powered system being activated. Comparisons to recorded seismograms demonstrate that the maximum warning times before potentially damaging shaking (intensity 6+) were in the range of 5–55 s. Although the ShakeAlert system provided accurate solutions and useful alert delivery, this earthquake raised awareness of potential issues within the system, including the need for improved offshore location estimates, a combination of solutions from ShakeAlert servers, and handling of spurious triggers.

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Journal
Bulletin of the Seismological Society of America
Published
2026-04-17
DOI
https://doi.org/10.1785/0120250232
Primary Topic
Seismology and Earthquake Studies
Type
article
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article

ShakeAlert Earthquake Early Warning System Performance During the Mw 7.0 Offshore Cape Mendocino Earthquake

J. K. Saunders, D. E. Smith, Sydney N. Dybing, Maren Böse et al.
Bulletin of the Seismological Society of America
Seismology and Earthquake Studies
article

ShakeAlert Earthquake Early Warning System Performance During the Mw 7.0 Offshore Cape Mendocino Earthquake

J. K. Saunders, D. E. Smith, Sydney N. Dybing, Maren Böse, Carl W. Ulberg, J. J. McGuire, Angela Lux, Robert De Groot, Stephen Crane, Sumant Jha, J. R. Murray, R. M. Allen, Jacob Crummey
article en

Abstract

ABSTRACT The 5 December 2024 Mw 7.0 Offshore Cape Mendocino earthquake was a challenging test of the U.S. West Coast ShakeAlert earthquake early warning system due to its offshore epicenter and limited near-source station coverage. We analyzed real-time performance of all components of the ShakeAlert system, including the seismic algorithms (earthquake point-source integrated code [EPIC] and Finite-fault rupture Detector [FinDer]), the geodetic algorithm (Geodetic First Approximation of Size and Time–peak ground displacement [GFAST-PGD]), and network telemetry during the event. EPIC created the first solution for this earthquake 15 s after origin time with an initial magnitude estimate of M 5.6 and location error of 10 km from the Advanced National Seismic System epicenter. An early spurious trigger from station CE.89101 fortuitously maintained location accuracy and, correspondingly, magnitude accuracy. FinDer contributed its first solution at 18 s with a location estimate closer to the seismic network and produced two distinct rupture geometries, leading to minor fluctuations in estimated intensity contours. GFAST-PGD did not meet alerting thresholds but otherwise performed as expected. Network latencies were <2 s for most stations, supporting the rapid detection of this earthquake by the system. Roughly five million alerts were delivered to cell phone devices in California and Oregon during this event. This was also the first instance of a school district-wide ShakeAlert-powered system being activated. Comparisons to recorded seismograms demonstrate that the maximum warning times before potentially damaging shaking (intensity 6+) were in the range of 5–55 s. Although the ShakeAlert system provided accurate solutions and useful alert delivery, this earthquake raised awareness of potential issues within the system, including the need for improved offshore location estimates, a combination of solutions from ShakeAlert servers, and handling of spurious triggers.

Bulletin of the Seismological Society of America
California Institute of Technology (US), Natural Resources Canada (CA), United States Geological Survey (US), Universities Space Research Association (US), Berkeley College (US), University of Washington (US), ETH Zurich (CH)
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Seismology and Earthquake Studies
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