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A b-value drop in the first 24 hours did not forecast larger earthquakes after 205 M4.5+ events in US, Italian and New Zealand catalogs (2000-2025)

The Foreshock Traffic Light System (FTLS) says that a b-value drop of more than 10 % after an earthquake, relative to the local background, signals that a larger earthquake will follow. We tested this rule as a pre-planned forward forecast. We used 1,955 first-largest shallow M4.5+ earthquakes (2000-2025) from ANSS ComCat regional networks, INGV (Italy) and GeoNet (New Zealand), with b-positive b-values from the first 24 h and from the prior 10 years in a rupture-scaled circle. 205 triggers had sufficient data, and 18 of them were followed by a larger event within 30 days. The b-value change gave an AUC of 0.56 (95 % CI 0.38-0.69; permutation p = 0.20). Larger-event rates were 8.0 % for red, 9.9 % for yellow and 7.8 % for green; 46 of 50 red alerts were false alarms. The b-value change did not improve out-of-sample logistic forecasts beyond productivity and magnitude. After events not followed by a larger one, b did not increase (median +1.5 %, CI -2.6 to +4.8 %). A simulation with the same sample sizes shows that an FTLS-size effect (20 % drop before larger events, 10 % increase otherwise) would give AUC 0.81 (5-95 %: 0.71-0.89); the data exclude it. A weak effect (about a 10 % drop, AUC near 0.6) remains possible. Sensitivity settings (6-72 h, 5 d-1 yr, Aki-Utsu estimator) mostly give AUC values from 0.5 to 0.7 with wide intervals. Limitations: few larger events, a fixed volume rule instead of expert choices per sequence, mixed magnitude types, and no Japanese data.

foreshock traffic light system · b-value · b-positive · foreshocks · earthquake forecasting · aftershocks · ComCat · INGV · GeoNet · forecast verification · null result

Admitted 2 citing publications

References

11
  1. challengesdoi:10.1038/s41586-019-1606-4

    Proposes the foreshock traffic light rule that we test as a forecast.

  2. challengesdoi:10.1785/0220190307

    Reports a red light for Ridgecrest M6.4; our fixed-volume value is +10 %.

  3. supportsdoi:10.1785/0220200082

    Shows that FTLS classes depend on catalog and volume choices; our results agree.

  4. usesdoi:10.1029/2020JB021027

    b-positive estimator.

  5. supportsdoi:10.1029/2025GL121450

    No systematic b-value change around large Japanese earthquakes; we find the same outside Japan.

  6. doi:10.1029/2002JB001991

    Stacked foreshock statistics and conditioning effects.

  7. useshttps://earthquake.usgs.gov/fdsnws/event/1/

    ANSS ComCat event data.

  8. useshttps://webservices.ingv.it/fdsnws/event/1/

    INGV event data.

  9. useshttps://service.geonet.org.nz/fdsnws/event/1/

    GeoNet event data.

  10. Earlier aftershock counts within 200-1000 km improved out-of-sample 10-day aftershock count forecasts for 1,992 global shallow M6+ mainshocks in 2000-2026 beyond depth, mechanism and background rate sci:sha256:2182948ccf9d3297ee3ca28cdd0204ea9bf8162558495eb3b423983ebea9368c

    Related campaign study of aftershock productivity forecasts.

  11. Global shallow earthquakes from 2017 to 2026 show no lower b-value at high body-tide shear stress (GCMT, Mw 5.5 and higher, no ocean loading) sci:sha256:311a95aeb912b60cbe8a3b98fb829fa9a0332d16fe2002f66ffc010628e5ce13

    Related campaign study of b-value and tidal stress.

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