
type things....mammatus clouds

mharratsc wrote:Reminds me of what the anode tufts look like on the Sun... o.O
webolife wrote: Why do clouds coalesce water vapor rather than diffuse it, in light of the fact that small condensing vapor molecules are generally negatively charged? Shouldn't the electrical repulsion between the droplets prevent them from forming clouds at all? But what is being observed in laboratory experiments is that the surface of water, including surface tension, but also situations like water vapor condensing around nuclei of condensation in the atmosphere [which nuclei are also negatively charged, this being a surprise to me, webolife] creates a layer of positive charge around it, [which Pollack refers to as] the exclusion zone or EZ. When two or more droplets are in the vicinity of each other, this positive charged EZ is increased in the zone just between the particles, creating a region of neg/pos/neg in which the neg charges actually attract toward each other, as Feynman said, "Like likes like."
When two or more droplets are in the vicinity of each other, this positive charged EZ is increased in the zone just between the particles, creating a region of neg/pos/neg in which the neg charges actually attract toward each other, as Feynman said, "Like likes like.
.What we have now is a coherent medium, something like a laser,..
FromWhat part does the jet stream play in tornado formation? Meteorologists have known that the long swift river of air called the jet stream has helped breed tornadoes in conjunction with masses of warm air and of cold air. They have long suspected the arctic jet stream that sweeps down from Canada as a major factor in producing U.S. tornadoes, but photographs from a space satellite in 1968 provided conclusive evidence that the sub- tropical jet streams sweeping out of the Pacific Ocean through Mexico play a major role in the creation of tornadoes.
Electric Currents Accompanying Tornado Activity
Marx Brook
Science
New Series, Vol. 157, No. 3795 (Sep. 22, 1967), pp. 1434-1436
(article consists of 3 pages)
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/1723338
Abstract
Measurements of the magnetic field and earth current in the vicinity of a tornado show large step-like deflections coincident with the touching down of the funnel. Calculations with a simple current model indicate that a minimum current of several hundred amperes must be postulated to account for the observed deflection in magnetic field. The existence of a steady current of 225 amperes for a period of about 10 minutes provides joule heat at the rate of approximately 10$^{10}$ joules per second, and involves a total charge transfer of 135,000 coulombs. The calculations imply that a tornado is electrically equivalent to several hundred isolated thunderstorm cells active simultaneously.
mharratsc wrote:See- THAT is what I was talking about! That was the point that I was trying to make with Charles Chandler in the other tornado thread we had going, but there wasn't any data to support the sustained current flow.
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