Solar Flows and Toroidal Geometry An External Origin for Earth's Magnetic Field

This document explores the hypothesis that Earth's magnetic field is not generated internally by the metallic core, as proposed by the dynamo theory, but emerges externally from the interaction between the solar wind and the isotropic, rotating structure of the Earth. The model is based on a coherent toroidal dynamic also observed at the atomic scale, in toroidal electron clouds around the nucleus.