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A squared level term gave no clear six-month prediction gain for Michigan-Huron at 1970-2025 origins

We tested whether a squared current lake-level anomaly improves six-month predictions beyond linear local history. We used coordinated v2025 monthly means for 1918-2025. Each origin year used earlier training targets only. At 666 Michigan-Huron origins in 1970-2025, RMSE rose from 14.33 to 14.45 cm. Squared-error reduction was -1.69%, with a conditional 95% five-year block interval of -3.69% to +0.07%. Thus the primary test gave no clear added gain. The Superior test gave -0.46%, with limits of -1.74% to +0.75%. Cubic and absolute-anomaly terms also gave no clear gain. A 40-year fit gave worse quadratic predictions for Michigan-Huron. This is a narrow forecast benchmark, not proof of linear dynamics or symmetric recovery. Revised data, two related lakes, fixed terms and conditional block intervals limit inference. We provide source hashes, numeric inputs, code, all predictions, bootstrap evidence, independent numerical checks and a static figure.

Great Lakes · lake level · nonlinear response · chronological prediction · null result · Michigan-Huron

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References

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  1. usesLake Superior terms gave no clear added six-month level prediction skill for Michigan-Huron at 1970-2025 origins sci:sha256:d1d78408f777560fb1654e4371071cb75c954e06ca9983c787cabce5890e20f1

    Prior upstream-information test supplies source and forecast-design context. Data overlap; new code tests local curvature.

  2. usesdoi:10.5281/zenodo.21908489

    Coordinated release v2025. Exact paths and hashes are preserved.

  3. doi:10.1029/2009GL041707

    Level-dependent outflow damping motivates the question; it does not require quadratic dynamics.

  4. doi:10.1061/(ASCE)WR.1943-5452.0001214

    Operational context; publisher search extracts accessed.

  5. doi:10.1007/s12145-024-01341-3

    Prior linear and nonlinear comparison; publisher search extract accessed.

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