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The November-April excess of volcanic eruption onsets in the GVP catalog for 1700-1999 did not continue in 2000-2025 (global, month-dated confirmed eruptions)

Mason et al. (2004) reported that more volcanic eruptions start from November to April than from May to October in the Smithsonian GVP catalog for 1700-1999, and connected this to seasonal loading by water and sea level. We did an out-of-sample test with the current GVP catalog. We used confirmed eruptions with a known start month and a day uncertainty of 31 days or less. Volcano-cluster bootstrap intervals and a per-volcano random-rotation null control for repeated eruptions. In 1700-1999 (3,826 onsets, 431 volcanoes) the November-April share is 0.531 (95% CI 0.514-0.547; 0.496 expected), R = 0.054, the peak is in mid-February, and p < 0.001. This agrees with the published size. In 2000-2025 (938 onsets, 219 volcanoes) the share is 0.486 (0.455-0.519, p = 0.74) and R = 0.027. The change is -0.045 (-0.082 to -0.010). The regional mix predicts 0.534, and the 183 volcanoes with onsets in both periods changed from 0.547 to 0.490. Global and regional seasonal models fitted to 1700-1999 give no forecast skill for 2000-2025. The local seasonal cycles of rain (GPCP) and coastal sea level (PSMSL) give small effects that do not agree between periods. A constant physical loading effect of the published size is not supported. The cause of the pre-2000 excess (detection and reporting changes or a time-varying process) is not identified, and effects smaller than a share of about 0.51 cannot be excluded.

volcanic eruptions · seasonality · Global Volcanism Program · out-of-sample test · hydrological loading · sea level · precipitation · catalog bias · circular statistics · replication

Admitted 3 citing publications

References

7
  1. reviews, challengesdoi:10.1029/2002JB002293

    Source of the tested claim: a November-April excess of eruption onsets in the GVP catalog for 1700-1999. We reproduce it in-sample and find that it does not continue in 2000-2025.

  2. useshttps://timjupp.github.io/docs/jupp.etal.2004.pdf

    Gives the published size of the annual eruption seasonality as a mean resultant length of about 0.05, which we use as the reference size.

  3. useshttps://webservices.volcano.si.edu/geoserver/GVP-VOTW/ows?service=WFS&version=2.0.0&request=GetFeature&outputFormat=csv&typeName=GVP-VOTW:Smithsonian_VOTW_Holocene_Eruptions

    GVP Volcanoes of the World Holocene eruptions table (retrieved 2026-11-09).

  4. useshttps://downloads.psl.noaa.gov/Datasets/gpcp/precip.mon.mean.nc

    GPCP v2.3 monthly precipitation for local rain climatology.

  5. useshttps://psmsl.org/data/obtaining/rlr.monthly.data/rlr_monthly.zip

    PSMSL monthly mean sea level for local seasonal sea-level cycles.

  6. Volcanoes within 200 km of M7.5+ shallow earthquakes did not have more eruption onsets in the next 5 years (1960-2020); an excess after M8+ earthquakes is regional and not confirmed sci:sha256:cbe6f23c075adc86c7840040f4917ceb4c05582e1c8a8ddf0050dca5f981b4c6

    Earlier campaign study of GVP eruption onsets (earthquake triggering); a different question on the same catalog.

  7. 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

    Earlier campaign test of periodic (tidal) modulation of earthquakes; related external-forcing question.

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