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The Vorticees of Tornadic Activity.
Vorticeeing is Believing. Click to go there.
The phenomena involves the break-up of spinning wind sheer indicating the involvement of swell movement at the boundary of terrestrial thermal layers in the troposphere. The vortices verticise causing at least a significant part of tornadic activity. The spiral tends to emulate alternate gravitational orbiting vectors smaller than the curve of the earth upon which the parallel originates, causing it to tend to bow at intervals. Multiples may be the result of a longer parallel, such as in a large dry line in a larger weather system, sometimes more indicative of cooler seasonal conditions, such as Springtime-like ones. A large part is played by the polysubstantive nature of the atmosphere as it goes from probable dimensional changes from outer to inner levels of a sphere. Then these variant substantives of the same atmosphere "break" (as in a breaking wave at a seashore) when the swell at their thermal layer is one-seventh the size of the then layer's distance to the ground, sometime resulting in the vertization of the vortex after the shrinking of the orbital vector from planetary to secondary gravitational bowing, connecting the biosphere with the stratosphere. It shows a dimensionable relationship between two of the new dimensions I have discovered which I label "magnitude" and "mineatude". It also illustrates it's relevance to the other perpetuation forces such as gravitation and magnetism which may be all the same phenomenon. This is observable in objects disintegrating upon entry into the atmosphere from space. The object can safely enter only if it can alter it's state from a magnitudinal to a lesser magnitudinal or mineatudinal state. Click here to return to "Proxemics". Click here to return to "Orbiting Vectors".
... spinning wind sheer
following a principal of mineatudinal gravitation ... |