Planetary Core Dynamo Feedback (PCDF)

Solar-Linked Electromagnetic Torque as a Driver of Core Dynamics

Intellectual Property Protected | First Authored 2023

Overview

The PCDF model proposes that Earth's planetary core is influenced by internal convection, rotation, atmospheric coupling, and electromagnetic torque introduced through coupling with the solar magnetic field. The Earth's atmosphere — through global lightning discharge, Schumann resonances, and telluric current systems — forms a reactive shell that insulates and interacts with the geomagnetic field and deep Earth dynamo. This coupling forms an integrated feedback system that subtly regulates the Earth's rotation rate, magnetic reversals, and seismic triggering through complex core-mantle-atmosphere interactions.

Origin Note

"The Sun's magnetosphere wraps around Earth like a thread on a needle. What if that thread does more than just wrap — what if it pulls? When the Earth is struck by solar energy, I believe more of it is absorbed and dispersed throughout Earth's atmosphere and core dynamo."
— Shelton Rusie, March 2023

This idea marked the first instance of conceptualizing the Sun's magnetic field as an active driver of planetary core modulation instead of a passive environmental effect.

Core Concepts

Downloadable Materials

📄 Whitepaper

Full theory document on PCDF

Coming Soon

📎 PPA Document

Provisional Patent Filing (planned)

Not Yet Filed

🛰️ arXiv Preprint

Journal-style manuscript in progress

Coming Soon

Related Theories

This model complements the following frameworks:

Coming Soon

Field Equation Appendix: Full PDF of rotational and vector torque models
Observational Correlation Log: SYM-H index comparisons with L.O.D. anomalies and seismic upticks
Experimental Proposals: New avenues for correlating solar wind data with deep-core simulations

Contact

Interested in collaboration, simulation, or licensing?
📬 Contact Me