THE BIVORTEX IN CYCLONES & TORNADOES
Copyright 2007 George William Kelly

A tornado on the advancing edge of a massive cyclone is like a tiny cogwheel turned by a gigantic cogwheel.

The huge difference in ratio between the two "cog wheels" transfers the tremendous power of a cyclone into the high speed and devastation of relatively small tornadoes.

Tornadoes are known to occur in strings along the advancing, rotating edge of a large cyclonic storm system. The tornadoes descend from smaller "cell storms" (baby cyclones) that form along the circumference of the large cyclonic system when the system shears against an opposing air mass.

The central tornado of a cyclone is the lower of two bipolar jets shot out from the top and bottom of the "cell storm's" eye--similar to bipolar jets shot out by certain types of stars. The upper jet from the "cell" aborts harmlessly into the thin, dry stratophere, but the lower jet becomes a vicious tornado when it descends through warm, moist air and strikes the ground.

We believe that hurricanes, typhoons, cyclones, and tornadoes are "bivortex" bodies that follow the same bivortex field pattern as atomic protons, stars, and galaxies. All are composite bodies, each made up of smaller particles that move in recirculating paths to create a doughnut-like or spherical shape resulting in a quadrupole gravitoelectromagnetic field.

A bivortex is comparable to the shape of an apple, with a north pole funnel or vortex, a south pole vortex, and a central core. The smaller particles spiral into the polar vortexes, collide at the core's center, bulge out at the equator, then arch back again toward the core and vortexes. When the apple spins too fast, the smaller particles jet out of the two poles. In the case of stars the bipolar jets extend thousands of light years into space. With tornadoes, one jet quickly strikes the ground below and creates havoc.
- posted by George William Kelly @ 9:08 PM