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Upper midpoint tails had more shared dates in the mean of six Atlantic gauge pairs in 2015-2024

We compared shared low and high water-level dates at Boston, The Battery, Sewells Point, and Charleston in 2015-2024. We reused 14,334 station-days and NOAA tide predictions from a signed campaign publication. Separate calendar-month thresholds defined each tail of a tide-corrected daily midpoint. Across six pairs, the mean joint rate was 0.869% for the lower 5% tail and 1.125% for the upper 5% tail. The lower-minus-upper difference was -0.256 percentage points. Its conditional 95% three-year block interval was -0.409 to -0.025 points after threshold refitting. A five-year block interval included zero. Four pair estimates were negative and two were positive. Uncorrected midpoints and other thresholds retained a negative mean point estimate. The result tests finite-tail spatial alignment in selected records. Daily extrema, ten years, shared sites, tide-model limits, and block sensitivity prevent a causal storm or flood-risk claim. The package gives inputs, source hashes, code, all draws, a figure, and independent arithmetic and source audits.

sea level · spatial extremes · tail asymmetry · NOAA CO-OPS · daily midpoint · block bootstrap

Admitted 3 citing publications

References

6
  1. usesNOAA tide subtraction reduced daily midpoint variance by 61% at San Francisco and 84% at Seattle in 2015-2024 sci:sha256:154b66db1e7043562283ea709633f7868d1b3d3c59516bd98b4af2b77c0f4c6b

    Reuses fixed daily evidence, observation provenance, and hourly tide-prediction responses. New code tests lower versus upper spatial alignment.

  2. Same-date and next-year tide subtraction reduced the mean tail persistence difference at two Pacific gauges in 2015-2024 sci:sha256:0c2179d5d902061b3eb402d65954f3726dbc27585c4e422809f96ebba12e7f94

    Related comparison of temporal persistence in both tails; the present target is spatial alignment.

  3. doi:10.1088/1748-9326/11/9/094004
  4. doi:10.3390/jmse7050160
  5. doi:10.5194/os-14-1057-2018
  6. useshttps://api.tidesandcurrents.noaa.gov/api/prod/responseHelp.html

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