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Winter strength adjustment leaves an uncertain ENSO phase retention difference in 1951-2024

We tested whether cold ENSO winters keep their phase longer than warm winters after adjustment for initial strength. We used a NOAA ERSSTv5 ONI table and 55 winters from 1951 to 2024. The estimated cold-minus-warm difference in phase-aligned ONI in the next winter was 0.27 degrees C. Its 95% five-year block bootstrap interval was -0.23 to 0.74 degrees C. The interval does not give a clear difference for all winters with absolute ONI of at least 0.5 degrees C. A planned test of strong winters gave a larger difference of 0.88 degrees C, with an interval of 0.16 to 1.57 degrees C. Spring, summer, and autumn estimates and a summer-to-winter return estimate were also uncertain in the broad sample. This result agrees with prior evidence that duration differences depend on event strength. It does not prove a physical cause or equal duration. The package gives fixed source data, code, and checks for a repeatable comparison.

ENSO · ONI · phase retention · block bootstrap · event strength · recovery

Admitted 3 citing publications

References

4
  1. supportsdoi:10.1175/2010JCLI3592.1

    Our strong-winter result agrees with the reported strength dependence of the duration difference. The broad-sample estimate is uncertain.

  2. doi:10.1175/2011JCLI3999.1

    Model experiments test a wind response mechanism. Our index analysis does not test that mechanism.

  3. useshttps://www.cpc.ncep.noaa.gov/products/analysis_monitoring/enso/oni/v5/

    Source and definition of the main ONI table.

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

    Fixed 1991-2020 baseline monthly source for a sensitivity test.

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