Proposals to Recalibration and Dynamics in Earth's Rotation: Through the lens of ITF
Abstract
UNDER EDIT. We present empirical evidence for electromagnetic coupling between Earth's rotational and magnetic axes as the primary mechanism sustaining planetary rotation against tidal friction losses. The optimal coupling angle of 13 derives from the Informational Topography Field (ITF) lattice displacement ratio δ = 0.13, a fundamental geometric constant governing spacetime structure. Analysis of magnetic pole position data spanning 1900-2023 reveals statistically significant correlation (Pearson r = 0.534, p = 0.0401) between deviation from this optimal angle and magnetic pole velocity, confirming the theoretical prediction. The system achieved maximum coupling efficiency in 1990 when the magnetic axis was positioned at 11.7 from the rotational axis, representing the closest historical approach to the theoretical optimum. Current deviation of 9.2 correlates with unprecedented magnetic pole acceleration of 58.4 km/year, representing a 4.2-fold increase over the 1900-1980 historical average. We propose Earth undergoes periodic electromagnetic recalibration events triggered by coupling degradation beyond critical thresholds, manifesting as crustal fracturing, deep hydrate expulsion, continental reorganization, and biological transitions. The ITF lattice framework explains these phenomena through geometric first principles, offering a unified model connecting cosmological structure formation, planetary electromagnetic dynamics, ocean chemistry evolution, and biological renewal cycles. The core hypothesis proposes ultra-high-pressure hydrated silicate phases rather than iron-nickel composition, with piezoelectric field generation providing direct coupling between rotational stress and magnetic field evolution. Periodic dehydration events expel water and dissolved halides to the surface, explaining oceanic chloride excess and providing the mineralogical and chemical basis for renewed organic synthesis. Statistical extrapolation of current trends indicates continued system instability through 2026-2027, with testable predictions for observable electromagnetic phenomena, seismic activity patterns, and rotational anomalies. The framework provides falsifiable criteria distinguishing it from standard geodynamo models.
Fields of Study & Subjects
Geomagnetism and Paleomagnetism Studies
Earth Systems and Cosmic Evolution
Geophysics and Sensor Technology
Publication details
- Publication date
- 16 January 2026
- Document type
- Preprint