tornadoes

TORNADO DYNAMICS

Tornadoes happen after geomagnetic storms when the interface between the high density polar air mass and ambient mid latitude air mass is across the US midwest. The increase in charge density and repelling force between electrons in the electrified sectors of the auroral ovals powers a high velocity shock wave which increases barometric pressure and wind speed along the interface with the mid latitude air mass.

May 17, 2013 – M3 Class solar flare and geoeffective CME
May 18 -19, 2013 – Over the weekend, a pair of CMEs hit Earth. The impacts sparked Northern Lights visible as far south as Colorado. Some of the brightest appeared over Cape Cod, Massachusetts.

May 20, 2013 – TORNADOES KILL 24 & INJURE 212 when an EF5 tornado ravaged Moore, Oklahoma, and adacent areas, with peak winds at 210 miles per hour, part of a larger system which produced several other tornadoes across the Great Plains over the previous two days, including five that struck portions of Central Oklahoma on May 19.

The increase in wind speed increases the momentum of storm fronts and the Coreolis Force powers anticlockwise rotation of storm cells of ionized droplets which transform the angular momentum of moving charges into moments and sum of moments into a dipole field along the rotation axis which attracts cloud droplets toward the ground.

supercell hook

Storm fronts trap electrons on cloud and ground surfaces which induce like charge in the same instant on field lines of twin phase electrons which drape cloud and ground surfaces between cycles. Like charges induced in the same instant are electrically repelled and cloud electrons repel ground charge from rainshadow surfaces, inducing a voltage potential which attracts cloud electrons to rainshadow surfaces.

The anticlockwise vortexes of ionized cloud droplets transform the momentum of spiralling charges into a field along the rotation axis which is attracted to the charge of rainshadow surfaces and attracts vortex droplets toward the ground.

When a vortex touches the ground circuits are opened between field lines draping cloud vortex and ground surfaces and the vortex field attracts a high amperage current surge of ground charge up vortex field lines which transform the momentum of spiralling charges into moments which catastrophically increases the attractive force of the dipole field and transforming the vortex into a tornado.

Tornado dynamics

JULY 9-11 2013 – STRONG CIRCUMPOLAR AURORAS
JULY 10 2013 – 5000 LIGHTNING STRIKES IN IDAHO
JULY 11 2013 – 1500 STRIKES IN CORLORADO IN 24 HOURS –
JULY 11 2013 – TORNADOES KILL SIX IN NORTH TEXAS –

SEPT 30 2013 – HIGH SPEED GEOEFFECTIVE CME
OCTOBER 2 2013 – G2 CLASS GEOMAGNETIC STORM
OCTOBER 4 2013 – During the afternoon hours a large and violent multiple-vortex tornado moved across several counties located in rural Nebraska. The tornado injured fifteen and inflicted $50.5 million (2013 USD) in damages along a 18.94 mi (30.48 km) path.

Dec 8th 2023 – SOLAR FLARE & EXTREME UV FLASH:
DEC 10 2023 – Tennessee tornadoes leave at least 6 dead, dozens hurt and more than 35,000 without power.

June 15, 2023 – G2-CLASS GEOMAGNETIC STORM:
June 15, 2023 – TORNADO HITS TEXAS Texas town devastated by tornado, 5 dead across South from severe weather

March 23 2023 – 8 HOUR G3-CLASS GEOMAGNETIC STORM
March 24-27 2023 – TORNADOES ACROSS MISSISSIPPI ALABAMA & GEORGIA

March 31 2023 – GEOMAGNETIC STORM & BRIGHT AURORAS
March 31-APRIL 1 2023 – In all, 146 tornadoes touched down; 115 occurred on March 31 alone. The outbreak ranks third worldwide for producing the most tornadoes in a 24-hour period, with 136 tornadoes occurring between 19:00 UTC March 31 – 19:00 UTC April 1.

Dipole Moments