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Earth rotation slowing gave no forecast gain for global M≥7 earthquake counts in 2017-2025, and the 1900-2016 link was weak and absent at 10°N-30°S

Question: does a slowing of the Earth's rotation (length-of-day increase) come 5-6 years before more M≥7 earthquakes, as Bilham and Bendick said in 2017? They forecast 25-30 % more M≥7 earthquakes from 2017 for at least five years, with the strongest effect at 10°N-30°S. Approach: we used the IERS EOP C02 length-of-day series (1830-2026) and USGS ComCat M≥7 counts (1900-2025, 1,607 events), with ISC-GEM, M≥7.1 and Gardner-Knopoff declustered counts as checks. We used phase-randomised length-of-day surrogates as the null model, Poisson forecasts fitted on 1900-2016 for 2017-2025, and rolling one-year-ahead forecasts for 1950-2025. Results: 2017-2022 had 12.2 M≥7 earthquakes per year against a 1900-2016 mean of 12.7 (ratio 0.96, 95 % interval 0.70-1.25); 2017-2025 gave 1.03. All 24 models fitted on 1900-2016 forecast 2017-2025 worse than a constant rate. In 1900-2016 the best correlation at a 4-7 year lead was r = 0.22 (surrogate p = 0.07; p = 0.03-0.22 over 48 variants). At 10°N-30°S there was no relation (r ≤ 0.11, p ≥ 0.33). A post hoc relation north of 10°N (r up to 0.64) also failed out of sample. Rolling forecasts gained 0.20 nats over 76 years (surrogate p = 0.14). The fast rotation of 2016-2021 predicted fewer earthquakes in 2021-2025, but the mean was 15.0 per year. Limitations: only about four length-of-day cycles and nine new years, so an effect near 15 % cannot be excluded; we did not repeat the topological renewal-interval analysis.

length of day · Earth rotation · global seismicity · M7 earthquakes · earthquake forecasting · out-of-sample test · surrogate data · ComCat · ISC-GEM · IERS EOP C02 · replication

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References

9
  1. challenges, reviewsdoi:10.1130/abs/2017AM-300667

    Source of the tested forecast: 25-30 % more M≥7 earthquakes 5-6 years after rotation slowing, from 2017, strongest at 10°N-30°S.

  2. reviewsdoi:10.1002/2017GL074934

    Bendick and Bilham (2017) GRL; Figure 4a links length-of-day change to 10-year mean M≥7 counts. We test that link with surrogate nulls and out-of-sample data.

  3. useshttps://hpiers.obspm.fr/eoppc/series/longterm/eopc02.1830-now

    IERS EOP C02 combined UT1/LOD series, downloaded 2026-11-09.

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

    USGS ComCat and ISC-GEM (catalog=iscgem) M≥6.5 event lists, downloaded 2026-11-09.

  5. usesdoi:10.1111/j.1365-246X.1994.tb02471.x

    Jordi et al. (1994): source of the pre-1955 part of the C02 length-of-day series.

  6. doi:10.1785/0220140111

    Bragato and Sugan (2014): decrease of the northern-hemisphere M≥7 rate since 1900, relevant to catalog changes.

  7. Shallow M7+ earthquake pairs within seven days had excess spatial clustering under yearly shuffles in 1976-2025 sci:sha256:1509484abf83224f9dbf26796a30eb882d2aa10f04cfc2d9f5c095608647dc7a

    Related campaign test of temporal-spatial clustering of global M7 earthquakes.

  8. Shallow M7 pairs within 300 km showed no clear excess at 30-180 days under five-year shuffles in 1976-2025 sci:sha256:f3b28b9383e4ab52fa7a83ec0728269a08b4a961a2d6eaf7e46208e459eed730

    Related campaign test of M7 pair clustering at 30-180 days.

  9. A reported solar-wind density link to next-day M5.6+ earthquake counts in 1996-2016 depends on one day (2011-03-11) and did not repeat in 2017-2026 OMNI or SOHO data sci:sha256:2db4ca6a83f8841f3e8d639b47dbb18b6cb9ee38dce14b77402eb98da9991068

    Related campaign out-of-sample test of an external-forcing earthquake link (solar wind), with the same type of null result.

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