The Modern Solar Minimum And Geomagnetic Pole Reversal
Creators: name: Kirjonen, Miikka Markus
name: Kirjonen, Miikka Markus
Publisher: name: Zenodo
Year: 2025
Subjects: subject: dipolar coherence
subject: geomagnetic systems
subject: gravitational or magnetic anomalies.
subject: shape potential
subject: magnetospheric coupling
subject: magnetosphere
subject: the solar wind
subject: fractal wavefunction
subject: recursion
subject: curvature
subject: opposite angular momenta
subject: critical anisotropic axis.
subject: Earth's dynamic interior
subject: negentropic pocket
subject: dipolar magnetism
subject: Earth's core dynamics
subject: Earth
subject: Magnetic Pole Reversal
subject: Magnetic Pole Shift
subject: Solar Activity
subject: solar activity
subject: dynamo

description: RSM brings a unifying perspective on how solar and infinite adjacency terrestrial phenomena can become phase-locked through fractal recursion, ultimately shaping the local “negentropic pockets” that influence both climate and geomagnetic systems. In this paper, RSM serves as a conceptual backdrop, positing that reorganized phase-locked wavefunction pockets—driven by low solar activity—can shift local shape potentials that mimic gravitational or magnetic anomalies.

The geomagnetic field, predominantly generated by electrical currents in the Earth’s liquid outer core, experiences boundary conditions shaped by the solar wind. During Maunder-like epochs, reduced solar wind density and suppressed heliospheric turbulence can lead to diminished magnetospheric coupling, in turn moderating the dynamo effect. References [2,3] highlight how changes in cosmic ray flux and solar wind pressure can affect the outer boundary of Earth’s magnetosphere, thus subtly altering the delicate flows in the molten iron core. This causal chain resonates with our notion that external wavefunction perturbations—here, a quiet Sun—reconfigure local adjacency couplings, effectively retuning the Earth’s energy distributions. 

In our approach, energy reorganized by fractal wavefunction recursion can appear as an emergent local shape potential. Traditional treatments in general relativity express the spacetime curvature through 

Gμν = 8πG ⟨Tμν(Ψchiral)⟩, 

where Tμν(Ψchiral) depends on chiral fields or wavefunction alignments.
description: Chiral-Based Description Of Earth’s Dipolar Magnetic Field

In the RSM context, modeling the north and south poles as chiral entities with counter-rotating momenta is consistent with the idea that dipolar magnetism reflects two interlinked “vortical” wave states. By assigning each pole a quasi-wavefunction (ΨNorth and ΨSouth), then combining them via a tensor product and a global phase factor, we're effectively imposing the phase-locked condition that enforces dipolar coherence.

Ψearth Magnetic=ΨNorth Pole  ⊗  ΨSouth Pole  ⋅  e i ϕ(t)  ⋅  Θ(χEarth),

RSM’s approach;





Ψnorth Pole & Ψsouth Pole, We represent the north and south chiral states—each having opposite angular momenta. Their wavefunctions encapsulate local “vortical” features, effectively capturing the magnetized flow associated with each pole.




Exponent eiϕ(t), Applies a global phase factor that can vary in time, reflecting how these dipole states remain locked or shift in alignment. Ensures that small changes in local wavefunction amplitude or Earth’s core dynamics can be accounted for via ϕ(t).




Θ(χEarth), Imposes the critical-axis identification or “infinite adjacency” that RSM uses to unify both poles in an instantaneous feedback loop. Ensures that wavefunction changes at one pole are not independent but are reflected throughout the entire lattice.



Thus, we’re formally stating that Earth’s dipolar magnetic structure arises from two chiral wave states whose opposite angular momenta unify under near-infinite coupling along Earth’s “critical anisotropic axis.” This setup is consistent with the the notion that local resonances, fractal recursion, and partial dimension collapse can maintain stable negentropic pockets (in this case, the coherent dipolar geometry) despite the Earth’s dynamic interior.