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The Tornado

 

 

  
The Tornado
Books on the weather (Amazon.com)
Books on the weather(Amazon.co.uk)
Copyright Peter Thomson 2005
 

 

  1. Tornado Index
  2. Introducing the Tornado
  3. The Tornado at Touchdown - a natural charge sheath vortex
  4. A Self Organised Structure for the Tornado
  5. Parameters for vortex formation
  6. Charge Sheath Vortex - Plasma Theory
  7. Ball Lightning - natural fusion
  8. Controlled Nuclear Fusion from a Charge Sheath Vortex
  9. Fusion Powered Flight
  10. The Charge Sheath Tornado Controls Fusion in the Sun
  11. Charge Sheath revolution for Cosmology
  12. Flight 587 destroyed by a charge sheath vortex
  13. Charge Sheath dust storms on Mars

    Tornado Experiments

  14. Introducing the tornado experiments
  15. Modes of plasma charge sheath structures - torus

  16. A Charge Sheath Tornado in the laboratory
  17. A simple fusion gun

  18. The Charged Sheath Vortex Conference/ Discussion board

 

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Tornado Touch Down

How a Charge Sheath Vortex Explains the Observations

Large dust and debris clouds often obscure the processes at work at the ground.
But small tornadoes allow  a better view of the processes.

If you have examined the video clips of tornadoes on the previous page, you will have seen that the tornado tube forms in a rotating storm cloud, and descends to the ground.
Although rotating at high velocity, there is no outflow of air.
Debris and air is picked up at the base of the rotating core and accelerates rapidly upwards and outwards.
This airflow appears to expand rapidly, with moisture condensing outside the central core.


tornado at ground It appears as though the central core has a high electrical charge that induces the opposite charge onto everything near it. The attractive forces are huge and together with the abrasion of particles rotating in the sheath it rips the surface from anything it touches. As these ripped off particles start to speed up the particles that were violently attracted are now violently ejected.
tornado at ground
The rising cloud of ejected material accelerates and expands as it does so. This would suggest that this rising airflow is also now highly charged, but not attracted to the ground or the central core.

See the movie from http://redrock.ncsa.uiuc.edu/~jewett/Obs/May1598.html This is Overview This is a good sequence starting with charged sheath vortex touching down, clearly visible as a thin tube. An ejection cloud starts to build up and an outer turbulence vortex starts to form, but is then blown away - ahead of the vortex - by the surface wind. The outer turbulence vortex then reforms, and by the time it crosses the road is extremely well defined. At around 16 seconds part of the turbulence vortex is again breaking up in a large curl, again blown out by a wind moving faster than the vortex is travelling

Ejection Zone

If you watch a small tornado closely you can see these forces at work. Watch how the opposite charged dust from the ground is thrown out at high speed and then seems to drift downward again. This shows very clearly that at this stage there is almost no airflow coming down the tornado or going up the tornado. See the movie from http://www.uni-stuttgart.de/Wetter/specials/movies/tornado2.mpg Look at the time between 00.03 to 00.06 A small tubular charged sheath vortex is visible inside the larger turbulence vortex.


at ground 3

Charge Particle Expansion creates a Turbulence Vortex

As the ejected charged dust cloud increases, the charge between the dust and the charged air molecules create a pressure that forces the particles apart and reduces the density. This charge induced reduction in density makes the ejection cloud lighter than the surrounding air so it starts to rise.

As this dust cloud rises it draws air in from round the base of the tornado, and this rising air may also start to rotate, but at a much slower rate than the charged sheath vortex spinning at high speed inside it.

So what physical phenomenon can bring about this pattern of charge? See the next page.
 
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The Tornado - Severe Weather Systems