HIELO POSITIVO versus HIELO NEGATIVO

Los millones de cristales de hielo en el interior de un verdadero
cumulunimbus, están cargados por electricidad positiva y negativa .
Los cristales de hielo más pequeños tienen carga positiva y son
arrastrados a la parte alta de la nube. Los más grandotes
tienen carga negativa y ocupan la parte inferior de la nube.
Entre unos y otros se mantiene una energía de millones de voltios
y cuando chocan entre sí (siempre van pegando botes dentro del
cumulunimbus), se produce el rayo. Como en la fotografía.


O sea, que cuánto más hielo contiene un cumulunimbus, mayores
son los rayos o descargas eléctricas que este hielo produce.
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HIELO versus HIELO = RAYOS Y CENTELLAS

Esos trocitos de hielo en el interior de un cumulunimbus, formados a miles
de kilómetros de altura, cuando se golpean entre sí la nube revienta y
provocan una explosión eléctrica que cae en forma de rayo sobre la Tierra,
y, a su paso, su temperatura es
tres veces mayor que la de la superfície del Sol.




Sept. 13, 2006:

Here's something fun to try in your kitchen: Go to the freezer, open the door and pry loose an ice cube. Next, look around the freezing compartment for some frost—the crystalline fuzz that loves to coat your frozen English peas. Found it? Rub the ice cube gently across the frost.
Nothing happens.

Well, what did you expect, a bolt of lightning?

Actually, that's just how lightning gets started. Miles above Earth in cumulonimbus clouds, tiny ice crystals are constantly bumping against larger ice pellets. The two kinds of ice rubbing together act like socks rubbing against carpet. Zap! Before you know it, the cloud is crackling with electric potential—and a bolt of lightning explodes to the ground.

It may seem hard to believe that a powerful bolt of lightning, which heats the air in its path three times hotter than the surface of the sun, could spring from little pieces of ice. But that's how it is, according to theory, and indeed laboratory experiments have confirmed that you can generate electricity from ice-ice collisions.

Still, it does sound fantastic. So, "we decided to check it out," says Walt Petersen, a lightning researcher at the National Space Science and Technology Center in Huntsville, Alabama.
Over a three year period, Petersen and his colleagues used the Tropical Rainfall Measurement Mission (TRMM) satellite to look inside more than one million clouds. "TRMM has a radar onboard to measure the amount of ice in a cloud. And it has an optical detector called LIS (lightning imaging sensor) to count lightning flashes." By comparing the ice content of a cloud to its flashes, they could tell if ice and lightning really go together.

They do. "We found a strong correlation between ice and lightning in all environments—over land, over sea and in coastal areas." On global scales, the correlation coefficient between lightning "flash density" (flashes per square-kilometer per month) and "ice water path" (kilograms of ice per square-meter of cloud) exceeded 90%. Even stronger correlations were found on the smaller scale of individual storm cells where, for example, about 10 million kilograms of ice would produce one lightning flash per minute.
10 million kilograms. No wonder you couldn't get a spark going in your freezer. A great deal more ice is required to make lightning.
In a real thundercloud, millions of pieces of ice are constantly bumping together, pushed by updrafts ranging in speed from 10 to 100 mph. Tiny ice crystals become positively charged and waft to the top of the cloud, while bulkier ice pellets (called "graupel") become negatively charged and plummet to the bottom. This separation creates mega-volts of electrical tension--and hence the lightning.