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Winter ENSO did not reliably improve cherry bloom predictions at three sites in 1988–2025

We tested whether winter Niño 3.4 temperature anomalies add useful information to cherry bloom predictions at Kyoto, Liestal, and Washington. Each site had 75 annual records from 1951 to 2025. We fitted separate models with local time trends. We then predicted each year from 1988 to 2025 using earlier records only. Changes in mean absolute error were 0.039, -0.127, and 0.048 days, respectively. All paired five-year block bootstrap intervals included zero. All three full-period association intervals also included zero. An early association in Washington was weak in the later period. Quadratic trends and annual changes did not give clear full-period associations. These results limit the use of this simple ENSO predictor at these sites. They do not show that climate has no effect on flowering. Site changes, local weather, and pollution were not measured. The package includes source code, input hashes, aggregate results, and reproduction instructions.

phenology · cherry bloom · ENSO · temporal validation · observation bias · null result

Admitted 4 citing publications

References

5
  1. useshttps://github.com/GMU-CherryBlossomCompetition/peak-bloom-prediction/tree/a95298263523607c8489a7be091c8c8d8ce61979

    Fixed source of the three modern annual bloom records and their data notes.

  2. useshttps://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii

    Monthly ERSSTv5 anomaly series. Exact snapshot hash is in the package.

  3. reviewsdoi:10.1371/journal.pone.0027439

    Prior work on cherry bloom prediction from chilling and heat.

  4. reviewsdoi:10.1002/joc.1594

    Prior work on Kyoto flowering dates and spring temperature.

  5. reviewsdoi:10.2480/agrmet.52.163

    Prior work on ENSO and phenology in Asia.

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