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No-flow days at 137 US drying stream gauges did not rise past their 1999-2017 level in 2018-2025, except in western deserts and mountains; P/PET did not explain the shifts

Zipper et al. (2021) found that annual no-flow days at US non-perennial stream gauges changed in 1980-2017: drying in the south and west and wetting in the north. We tested if these changes continued in eight new climate years, 2018-2025. We used USGS NWIS daily discharge for 9,067 GAGES-II gauges and the same no-flow rule. We reproduced the published Mann-Kendall trend class for 96.8% of 539 matched gauges. Of 541 gauges with test data, 137 had a drying trend. In 2018-2025, 74% of these stayed above their 1980-2017 mean, but only 52% rose past their 1999-2017 mean (p = 0.73; median +1.5 days per year). In a placebo split inside the published period, 68% of drying gauges continued past their recent level in 2010-2017 (p = 0.002), so the stall is new. Wetting gauges continued a little (67% lower than their 1999-2017 mean, p = 0.002). Drying continued in the Western Deserts (13 of 16 gauges) and less in the Western Mountains. The 1999-2017 mean gave the lowest mean absolute error (29.0 days per year). Sen-trend extension (32.5) and a per-gauge model with basin precipitation over Thornthwaite PET (33.1) were worse. The climate model explained a median 33% of yearly variance. After the climate adjustment, 46% of drying trends and 70% of wetting trends stayed significant, and in 2018-2025 the trend gauges kept their offsets from the climate forecast. Thus, the changes acted as persistent level shifts that current- and prior-year P/PET did not explain. Limitations: only eight test years, near-zero discharge measurement sensitivity, most gauges are not reference gauges, temperature-only PET, and spatial clustering (HUC-2 cluster intervals include zero for some forecast differences). Code, derived public-domain tables, figures and source hashes are included. The CC BY-NC-SA Zipper et al. release is not bundled.

stream intermittency · no-flow days · non-perennial streams · out-of-sample test · trend persistence · USGS NWIS · GAGES-II · nClimGrid · aridity · replication · drought · hydrology

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References

7
  1. reviews, usesdoi:10.1088/1748-9326/ac14ec

    We re-test the 1980-2017 no-flow-day trends of this study with 2018-2025 data and use its no-flow definition and sample rules.

  2. usesdoi:10.4211/hs.fe9d240438914634abbfdcfa03bed863

    Zipper et al. data release (CC BY-NC-SA). Used only for aggregate replication statistics; not bundled.

  3. usesdoi:10.3133/70046617

    GAGES-II gauge list, attributes and basin boundaries.

  4. usesdoi:10.7289/V5SX6B56

    nClimGrid monthly precipitation and temperature for basin climate.

  5. useshttps://waterservices.usgs.gov/nwis/dv/

    USGS NWIS daily discharge, retrieved 2026-11-09.

  6. Runoff in 555 U.S. reference catchments did not stay low after 1,392 multi-year droughts (1951-2025) when annual precipitation and temperature are controlled sci:sha256:664b208cefa5e9bb1114a6ccf84255fc886f296b6f72198e385cbc30055fa7af

    Related campaign test of runoff persistence after droughts in US reference catchments.

  7. Linear trends fitted to 1941-2005 annual flood peaks gave worse 2006-2025 forecasts than a stationary model at 1,187 unregulated US gauges; carrying 30-40% of the trend gave only a 1% gain sci:sha256:9e64e735636c95e63afcade5982181f4c28f61e78da17ec27e8f3d2fb955907f

    Related campaign test in which 1941-2005 flood trends gave worse 2006-2025 forecasts than a stationary model.

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