Published April 2025 | Supplemental Material
Journal Article Open

ShakeAlert® Version 3: Expected Performance in Large Earthquakes

Abstract

The ShakeAlert earthquake early warning (EEW) system partners along with U.S. Geological Survey (USGS) licensed operators deliver EEW alerts to the public and trigger automated systems when a significant earthquake is expected to impact California, Oregon, or Washington. ShakeAlert’s primary goal is to provide usable warning times before the arrival of damaging shaking. EEW is most likely to achieve this goal in large‐magnitude earthquakes. In recent years, ShakeAlert has gone through a series of upgrades to its underlying scientific algorithms aimed at improved performance during large earthquakes. Version 3 of this software recently went live in the production system and includes improvements to all algorithms. The main seismic algorithms that detect an earthquake and characterize its location, magnitude, and fault rupture orientation are faster than older versions. Other key changes include: using real‐time geodetic data to characterize the magnitude growth in large earthquakes; the introduction of an alert pause procedure to compromise between speed near the epicenter and improved accuracy at larger distances; and the inclusion of a nonergodic site‐response model in the ground‐motion predictions. ShakeAlert has achieved its primary goal of usable warning times before strong shaking at some locations in real‐time operations in recent M 6 earthquakes. Using offline tests, we demonstrate usable warning times are possible for many sites with peak shaking values of modified Mercalli intensity (MMI) 7–8 in M 7+ earthquakes and also for many MMI 8–9 sites in M 8+ earthquakes. ShakeAlert partners use a variety of MMI and magnitude thresholds in deciding when to alert their users within bounds set by the USGS. Our study shows that there is room to raise the magnitude thresholds up to about M 5.5 without adversely affecting performance in large earthquakes. The ground‐motion criteria are more complex owing to a significant drop‐off in warning times between the MMI 4 and 5 levels of predicted shaking. However, widely used ShakeAlert products, such as the MMI 3 and 4 contour products, can provide sufficiently long warning times before strong shaking in moderate‐to‐great earthquakes to enable a range of protective actions.

Copyright and License

© 2025 Seismological Society of America.

Acknowledgement

Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This material is based upon work supported by the U.S. Geological Survey under Grant/Cooperative Agreement Number G21AC10525 to UC Berkeley, Number G21AC10532 to ETH Zurich, Number G21AC10523 to Central Washington University, Number G21AC10561 to Caltech.

Data Availability

ShakeAlert code is governed by an intellectual property agreement among the contributing authors. The ShakeAlert code is not publicly released. The Apache ActiveMQ software is available at https://activemq.apache.org (last accessed November 2024). The Apache Kafka software is available at https://kafka.apache.org (last accessed November 2024). ShakeAlert event summaries and parameters are available from the U.S. Geological Survey (USGS) via the contributor code “EW” through the National Earthquake Information Center’s (NEIC’s) catalog search tools at https://earthquake.usgs.gov/earthquakes/search/ (last accessed March 2024). ShakeAlert website https://www.shakealert.org (last accessed March 2024). All seismogram data used in this study are archived at either the Southern California Earthquake Data Center (Southern California Earthquake Data Center [SCEDC], 2013), the Northern California Earthquake Data Center (Northern California Earthquake Data Center [NCEDC], 2014), the Japanese National Research Institute for Earth Science and Disaster Resilience (National Research Institute for Earth Science and Disaster Resilience [NIED], 2019) or the EarthScope Consortium webservices (https://service.iris.edu/, last accessed December 2024). Data for the offline testing were obtained from the following seismic networks: (1) the AZ (ANZA; UC San Diego, 1982); (2) the BC (RESNOM; Centro de Investigación Científica y de Educación Superior de Ensenada [CICESE], Ensenada, 1980); (3) the BK (Berkeley Digital Seismic Network [BDSN], 2014, operated by the UC Berkeley Seismological Laboratory, which is archived at the Northern California Earthquake Data Center (NCEDC), doi: 10.7932/NCEDC); (4) the CC (Cascade Chain Volcano Monitoring; Cascades Volcano Observatory/USGS, 2001); (5) the CE (CSMIP; California Geological Survey, 1972); (6) the CI (SCSN; California Institute of Technology and USGS Pasadena, 1926); the CN (CNSN; Natural Resources Canada [NRCAN Canada], 1975); the IU (GSN; Albuquerque Seismological Laboratory/USGS, 2014); the NN (Nevada Seismic Network; University of Nevada, Reno, 1971); the NP (NSMP; U.S. Geological Survey, 1931); the NV (NEPTUNE; Ocean Networks Canada, 2009); the UO (PNSNUO; University of Oregon, 1990); the US (USNSN; Albuquerque Seismological Laboratory [ASL]/USGS, 1990); the UW (PNSN; University of Washington, 1963); and the WR (California Division of Water Resources). Geodetic data are available through Murray et al. (2023b) and NCEDC (2022). ComCat earthquake source information, ShakeMaps, and ShakeMap station observations were obtained from the U.S. Geological Survey (USGS, 2017, https://earthquake.usgs.gov/earthquakes/search/, last accessed January 2024). The supplemental material contains tables that describe the evolution of the ShakeAlert software (Table S1) and the test suite (Table S2). It also contains Figures S1–S6.

Supplemental Material

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Additional details

Created:
July 8, 2025
Modified:
July 10, 2025