Historical Test Cases

Overview

If Ӕ saturation governs tides, then major geomagnetic storms should leave measurable signatures in coastal tide records.

Amplitude or phase deviations (order centimeters) should align with storm onsets and recoveries.

These cases provide immediate, historical opportunities to test the prediction.

March 13, 1989: Hydro‑Québec Blackout Storm (Dst ≈ −589 nT, Kp = 9).

October–November 2003: The “Halloween Storms” (Dst ≈ −383 nT, Kp = 9).

August 4, 1972: Major storm associated with solar proton event (Dst ≈ −125 nT, Kp = 8+).

July 15, 2000: “Bastille Day” Storm (Dst ≈ −301 nT, Kp = 9).

September 1–2, 1859: Carrington Event (estimated Dst −850 to −900 nT, Kp equivalent 9+).

During each event, coastal tide gauges worldwide should show coherent, small departures from harmonic predictions.

Amplitude deviations: order 1–5 cm, especially near dip‑latitudes where EMF interaction is strongest.

Phase shifts: coherent with storm onset and recovery, not lunar/solar cycles.

Null expectation: conventional gravity model predicts zero effect, tides remain unaffected by space weather.

Select tide gauge datasets overlapping with the listed storm dates (NOAA, UHSLC, GESLA).

Compute Ӕ driver Σ(t) with and without geomagnetic framing (Kp/Dst).

Compare observed gauge residuals to harmonic baselines; test correlation with storm indices.

Confirm or falsify storm‑time tidal modulation.

These storms provide immediate test cases for the Ӕ law.

Prediction: tides flicker with the field, a phenomenon gravity cannot explain.Verification on historical data would be a decisive breakthrough.

Produced by The Lilborn Equation Team:

Michael Lilborn-Williams

Daniel Thomas Rouse

Thomas Jackson Barnard

Audrey Williams