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A count model gave no clear flood range score gain over past-error scaling at 83 US gauges in 2022-2025

We tested whether a negative-binomial count model improves annual high tide flood day ranges beyond a published past-error scaling rule. We used a verified NOAA table and 307 station-years at 83 US gauges in 2022-2025. Each test year used only earlier rows to fit one common extra-variance parameter. The mean was the NOAA range midpoint with a 0.5-day floor. The count model reduced the equal-year mean 68%-target interval score by 0.30 day against scaling. Conditional 95% limits were -1.21 to +0.47 days. Scores fell in three of four years. Counts inside the range rose from 59.3% to 72.0%, while mean width rose from 6.81 to 8.48 days. Removing 2023 changed the mean score difference to +0.13 day. The test therefore gave no clear score gain over scaling. The result is a count-model benchmark, not a new distribution or a physical explanation. Four test years, shared coastal errors, fixed possibly biased means, revised observations and inherited threshold checks limit inference. The resample limits hold fits fixed and omit serial dependence. The package includes frozen inputs, source hashes, every forecast, code, an independent scalar audit, sensitivity tests and a static figure.

high tide flooding · count model · negative binomial · interval score · chronological test · null result · coastal planning

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References

9
  1. usesNOAA annual high tide flood day ranges contained 57% of observed counts at 85 US gauges in 2019-2025, less than the 68% expected, and their midpoints did not beat a 5-year mean sci:sha256:067fb171353ce1ccadde578e2a2bff2474b78421a93efe886d5c096403aa75ca

    We reuse the verified 535-row stable-threshold table and its data provenance. The original records overlap; this is not independent confirmation.

  2. usesEarlier-year range scaling reduced high tide flood interval scores at 83 US gauges in 2022-2025 but covered only 59% of counts sci:sha256:fa7d38d960ffb6350d1762d9a0b2182523985b62ce1ded3ddbf366da9a4f56ba

    Its earlier-year range scaling is our primary benchmark. We add count-model intervals on the same test rows.

  3. useshttps://api.tidesandcurrents.noaa.gov/dpapi/prod/webapi/htf/htf_met_year_annual_outlook.json

    Shared frozen outlook snapshot of 9 November 2026; exact bytes and SHA-256 are included.

  4. https://repository.library.noaa.gov/view/noaa/70863/noaa_70863_DS1.pdf

    Documents the May-April target year and Pacific Island threshold changes.

  5. doi:10.1029/2018JC014741

    Prior coastal flood day count distributions with extra variance.

  6. doi:10.1029/2009WR007757

    Prior work on extra variance in annual river flood event counts.

  7. doi:10.3389/fmars.2022.1073792

    Prior prediction of coastal flood likelihood with tides and sea level inputs.

  8. doi:10.1198/016214506000001437

    Interval score used to charge for both wide ranges and misses.

  9. useshttps://docs.scipy.org/doc/scipy/reference/generated/scipy.stats.nbinom.html

    Mean-variance parameter form and distribution functions.

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