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TORNADOES Planetary field lines drop from the ionosphere current sheet eight times per second, draping and trapping static charge on cloud and ground surfaces between cycles and electrified storm cells of ionized droplets attract electrons, trapped on cloud surfaces which increases cloud, density and cloud electrons repel electrons from rainshadow surfaces and inducing a voltage potential attracting cloud electrons to rain shadow surfaces, and powers cloud to ground lightning strikes.
A U.S. map shows electrical currents in the ground at about 4:40 p.m. ET Thursday, when a geomagnetic storm hit G4 levels. These currents can lead to damage to the electrical grid. Read Less | NOAA Space Weather Prediction Center/U.S. Geological Survey/NOAA Space Weather Prediction Center/U.S. Geological Survey Tornadoes happen after geomagnetic storms when repelling forces between electrons powers a high velocity shockwave which increases wind speed and momentum of moving storm cells and the Coriolis Force powers anticlockwise rotation of storm cells of ionized droplets which transform the momentum of rotation into a dipole field which induces a voltage potential along the rotation access attracting cloud droplets toward the ground.
The momentum of spiralling charges transform into dipole moments which increases the rotation speed and dipole field propagating the funnel cloud towards the ground. When a funnel cloud touches the ground circuits open between field lines draping the funnel cloud and the ground and the voltage potential along the rotation, axis powers, a high amperage surge of ground charge up funnel cloud field lines.
The surge of ground charge, spiralling clockwise up field lines transforms the momentum of spiralling charges into moments which catastrophically increase the voltage potential along the rotation axis and velocity of cloud droplets spiralling towards the ground, transforming the spinning vortex into a tornado.
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