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Four-season rainfall fits retained a 2010-2019 runoff deficit at 70 Victorian gauges

We tested whether four-season rainfall terms remove a post-drought runoff deficit in CAMELS-AUS v2.03. We selected 70 Victorian gauges by fixed data coverage rules. We fitted annual and seasonal rainfall models to log-transformed annual runoff before 1997. In 2010-2019, the equal-gauge mean residual was -1.10 baseline standard deviations for annual rainfall and -1.02 for seasonal rainfall. The change was +0.08, with a conditional 95% spatial and time block interval of -0.09 to +0.26. The remaining seasonal residual had an interval of -1.61 to -0.46. Seasonal terms raised earlier held-out prediction error by 3.00% in the primary model. Checks with SILO rainfall, a linear annual response and stricter coverage retained negative mean seasonal residuals. This result limits one statistical explanation. It does not exclude other effects of rainfall timing or show a physical cause. Short records, model form, shared weather, data error and fixed fitted parameters limit inference.

Millennium Drought · Victoria · runoff · rainfall seasonality · model comparison · CAMELS-AUS

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References

5
  1. reviewsVictorian catchments that had not recovered from the Millennium Drought by 2017 stayed in a low-runoff state through the wet years 2020-2022 and to 2025 (143 gauges, annual hidden Markov models) sci:sha256:36d145c14c6ec974218c8e931718ed72d3cce8b76d5aec730e2ff5932212ff61

    Prior campaign test found low runoff after drought with annual rainfall models. We test a seasonal rainfall explanation with independent code and the CAMELS snapshot, not its derived evidence.

  2. usesdoi:10.5281/zenodo.14289037
  3. doi:10.5194/essd-17-4079-2025
  4. doi:10.5194/hess-26-6073-2022

    Prior work describes autumn rainfall loss as a possible cause of lower runoff.

  5. doi:10.1126/science.abd5085

    Prior study reports incomplete runoff recovery after the Millennium Drought.

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