WEATHER

WEATHER DYNAMICS

The planetary field captures electrons from the solar wind on field grounded in the atmosphere inside the auroral ovals which electrify sectors of the auroral ovals facing the night sky during geomagnetic storms. Electrons induce like charge in the same instant and like charges induced in the same instant are repelled with a force powering expansion of the electrified air mass air mass away from the pole.

The planetary field captures electrons from the solar wind which electrifies sectors of the auroral oval ovals facing the night sky during geomagnetic storms. The repelling force between electrons expands the high density air massd away from the pole, pushing back the ambient mid latitude air mass and increasing barometric pressure, wind speed and extreme weather along the jet stream interface.

Tornadoes happen shortly after geomagnetic storms when the interface between the polar and mid latitude air mass is across the US midwest. The sudden increase in charge density after storm powers a high velocity shock wave which increases wind speed along the interface where the coreolis force powers anticlockwise rotation of storm-cells of ionized droplets which transform the momentum of moving charges into dipole moments.