But for all we know, lightning might as well come from Zeus. Counting Ben Franklin's kite-and-key experiment as the starting point, 250 years of scientific investigation have yet to get to grips with how lightning works.
Atmospheric scientists have a basic sketch of the process. Positive electric charges build up at the tops of thunderclouds and negative charges build up at the bottoms (except for perplexing patches of positive charges often detected in the center-bottom). Electrical attraction between these opposite charges, and between the negative charges at the bottom of the cloud and positive charges that accumulate on the ground below, eventually grow strong enough to overcome the air's resistance to electrical flow.
Like a herd of elephants wading across a river, negative charges venture down from the bottom of the cloud into the sky below and move haltingly toward the ground, forming an invisible, conductive path called a "step leader." The charges' path eventually connects to similar "streamers" of positive charges surging up from the ground, completing an electrical circuit and enabling negative charges to pour from the cloud to the ground along the circuit they have formed. This sudden, enormous electric discharge is the flash of lightning.
But as for how all that happens — well, it just doesn't make much physical sense. There are three big questions needing answers, said Joe Dwyer, a leading lightning physicist based at the Florida Institute of Technology. "First, how do you actually charge up a thundercloud?" Dwyer said. A mix of water and ice is needed to provide atoms that can acquire charge, and updrafts are required to move the charged particles around. The rest of the details are hazy.
One theory holds that high-energy cosmic rays from space shoot down through the cloud, stripping off electrons from atoms as they go and dragging these negatively charged particles toward the cloud base, creating a charge imbalance. Dwyer said that although this process may play a role, it doesn't seem sufficient to explain the huge imbalance that scientists observe.
The consensus among scientists, he told Life's Little Mysteries, is that charge separation is mainly achieved in a process called "non-inductive charging mechanism."
"You have a mixed phase of ice and water up above 5 kilometers (3 miles) or so, and somehow those interact with each other and you have some kind of precipitation, and you have updrafts blowing up," he said. "Somehow the ice and water interact and manage to separate into oppositely charged particles. The lighter particles acquire positive charge and get blown to the top, and the heavier ones are negative and fall down."
That aforementioned positive patch near the bottom of the cloud remains a head-scratcher.
The second point of confusion is called the "lightning initiation problem." Measurements of the electric fields inside thunderclouds have consistently yielded peak values that are an order of magnitude weaker than is needed to break down the insulating properties of air. Man-made spark plugs require a much bigger electric field, or voltage difference between one electrode and the other in order for a current to tear across the gap. So the question is, "How do you get a spark going inside a thunderstorm? The electric fields never seem to be big enough inside the storm to generate a spark. So how does that spark get going? This is a very active area of research," Dwyer said.
Read more at Discovery News
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