Tombe, Frederick David
January 19, 2019
Coriolis force, magnetic field, Maxwell, vortices, aether, electron-positron sea, compound centrifugal force
The Coriolis force is a consequence of Newton’s first law of motion and it can be observed in a radial force field as a transverse deflection of the radial component of the motion by an amount required to conserve angular momentum. It is a physical reality most commonly associated with atmospheric cyclones, but it can also be observed deflecting the effect of gravity on a comet or causing a pivoted gyroscope to defy gravity. In a paper which he wrote in 1835 in connection with water wheels, French scientist Gaspard-Gustave Coriolis referred to its mathematical formula 2mv×ω as the “compound centrifugal force”. This is an interesting choice of name which suggests that it is the sum of two centrifugal forces, yet without giving any indication as to how this might be. The physical origins of the Coriolis force will now be traced to differential centrifugal pressure in the dense background sea of tiny aethereal vortices which serves as the medium for the propagation of light.