PHY 242 Net Research Project for 8/24/98



Lightning is a natural phenomena that occurs in almost every part of the world. It is the result of a large charge separation resulting from the friction between air masses sliding by one another. The lightning most people envision is between the ground and a cloud. Although the physics of ground to cloud lightning is the most understood, there are other more common types. And there are rare, fascinating examples, such as ball lightning. Ball lightning has a long written and oral history in sea folklore as the mysterious luminous glow that bounces about ships during unstable weather conditions. It is also one of the proposed explanations for the "spook light" that plagues my home area in southern Missouri.

If the weather is not too humid, you will be able to generate your own "safe" lightning bolts during this week's lab. You will use a Van der Graaff generator. Essentially, the Va der Graaff generator consists of a metal base, a fast moving rubber belt, and a metal sphere. Charge is transported from the base to the sphere by the belt. The Museum of Science in Boston has a very big generator that actually produces enough charge to be dangerous. The lightning link there shows how the initial lightning stroke is formed and why the visibility of the stroke usually moves upward. There are several links at this site worth exploring.

Red Sprite

Sprites (stratoshperic lightning) are another electrical discharge phenomena associated with thunder systems. They occur at the tops of thunder cells and extend into the stratosphere, reaching as high as 60 miles! The photograph to the left was taken by the Langmuir Laboratory Weather Center. The Langmuir GHCC Lightning Research Team also has a Lightning and Atmospheric Research site with all the latest of the research efforts. The Lightning Primer link has the latest information on sprites and a decent lightning tutorial, as well. (It takes some time to download, so be patient.) Although sprites are not well understood, there is evidence that they can effect chemistry in the stratosphere and create electrical disruptions in the ionosphere.

The questions are below. Don't forget that submissions are due by noon, Monday, Aug 31. Happy surfing!


Be sure to enter your full name. Enter your email address ONLY if you want the number of points awarded e-mailed to you. Responses should be brief but complete. You must click the SUBMIT button to submit your entry. Entries are due by noon on Monday of next week.



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