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Old December 16th 14, 07:45 PM posted to sci.geo.meteorology
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Default Vortex Phase: The Discovery of the Spin That Underlies the Twist

In a continuous loop, all the air in the troposphere eventually gets pulled up, funneled through the jet streams and allowed to fall back into the general flow. Laying along the boundary of the dry stratosphere above and the moist troposphere below, seven to twelve kilometers above our heads, jet streams are thermodynamic entities (previously unrecognized as such) that conserve energy and that, therefore, have 'spare' energy, which is itself the energy that causes storms. Jet streams possess genuine structural integrity.. They are a thing. More specifically, jet streams are naturally occurring conduits. Atmospheric pressure differentials accelerate wind down/through their tubular structures. Jet streams have the ability to grow both upstream and downstream. Sometimes, growing upstream, jet streams tunnel down to the lower part of the troposphere. When they do the resulting low pressure, atmospheric uplift, and condensation is what we observe as a storm. When a vortex grows all the way to the ground we call this a tornado. In this chapter I will tell you my solution to tornadoes. Specifically, I will tell you my prescription for how we can keep vortices up in the sky causing beneficial rainstorms and prevent them from growing all the way to the ground to cause death and destruction.

When I first mapped out the chapters in this book it was not my plan to provide this solution so soon. Rather it was my intention to, chapter by chapter, step you through the detailed arguments underlying such all-encompassing notions as, 1) how a flow along a common boundary of moist air (troposphere) and dry air (stratosphere) can come to possess genuine structural integrity, resulting in jet streams; 2) how recognition of jet streams as structural elements leads to a very simple, straightforward understanding of atmospheric flow, recasting the role of H2O to achieve a more complete and accurate conceptualization of the hydrologic cycle; and 3) how you yourself can verify the controversial sounding thinking being introduced herein, cutting through the well intended but superstitious rhetoric put forth by meteorologists and government paid tornado researchers. But then I realized that if I did all of this before the end or even the middle of the book I risked losing my audience before I had a chance to convey what I think is the most important message of this book that preventing large, destructive tornadoes will turn out to be unusually simple, inexpensive, and even mundane.

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