Unified Theory and Model of Planetary Instability on Earth Integration of Fluid Redistribution Core Fluid Dynamics and Magnetic Field Depletion from Iron and Nickel Core Mass Loss

Unified Theory and Model of Planetary Instability on Earth Integration of Fluid Redistribution Core Fluid Dynamics and Magnetic Field Depletion from Iron and Nickel Core Mass Loss: After aligningall variables exactly with Earth's factual datapoints, the dominant particaipant was the outer cores interaction. Changing viscosity of core by even .000001 would throw off wobble by weeks or months. That was the key to aligning the model. Run Simulations from 1995 to 2025. Find variables for 1995 and run the model forward and pay close attention to the core and axis of planet. After finishing and identifying all variables, specifically the outer core viscosity, I was able to run simulation from 1995-2025 and was able to replicate the Chandler Wobble reversal within hours of the actual recorded event. I invite all to challenge this theory and to simulate the finidings. All variable are inside the the paper to replicate the findings. I am still working on a Universal Model and hope to have that finished soon.

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-04-30
DOI
https://doi.org/10.5281/zenodo.15514729
Primary Topic
Lower Extremity Biomechanics and Pathologies
Type
article
Field-Weighted Citation Impact
0.00
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article

Unified Theory and Model of Planetary Instability on Earth Integration of Fluid Redistribution Core Fluid Dynamics and Magnetic Field Depletion from Iron and Nickel Core Mass Loss

Zenodo (CERN European Organization for Nuclear Research)
Lower Extremity Biomechanics and Pathologies
article

Unified Theory and Model of Planetary Instability on Earth Integration of Fluid Redistribution Core Fluid Dynamics and Magnetic Field Depletion from Iron and Nickel Core Mass Loss

article en

Abstract

Unified Theory and Model of Planetary Instability on Earth Integration of Fluid Redistribution Core Fluid Dynamics and Magnetic Field Depletion from Iron and Nickel Core Mass Loss: After aligningall variables exactly with Earth's factual datapoints, the dominant particaipant was the outer cores interaction. Changing viscosity of core by even .000001 would throw off wobble by weeks or months. That was the key to aligning the model. Run Simulations from 1995 to 2025. Find variables for 1995 and run the model forward and pay close attention to the core and axis of planet. After finishing and identifying all variables, specifically the outer core viscosity, I was able to run simulation from 1995-2025 and was able to replicate the Chandler Wobble reversal within hours of the actual recorded event. I invite all to challenge this theory and to simulate the finidings. All variable are inside the the paper to replicate the findings. I am still working on a Universal Model and hope to have that finished soon.

Zenodo (CERN European Organization for Nuclear Research)
Openalex Percentile: Top 56%
Lower Extremity Biomechanics and Pathologies
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