MadSci Network: Earth Sciences |
For all practical purposes, aurora and heat lightning are as different as ladybugs and pepperoni pizza. Heat lightning is merely regular old lightning which occurs far enough inside a cloud that its light is diffused throughout the cloud. We generally refer to this kind of lightning when the storm producing the lightning is well off in the distance toward the horizon (and clear sky may even be overhead). Thunderstorms rarely extend beyond thirteen to fifteen kilometres in height, the altitude at which the troposphere (the layer of the atmosphere beginning at Earth's surface) and the stratosphere meet. Lightning itself does not extend significantly beyond this height, though other phenomena related to thunderstorms may extend far into the stratosphere. However, these phenomena (known as elves and sprites) are very difficult to observe, and have only just recently been proven to exist. Aurora, on the other hand, occur at the outer extents of the Earth's atmosphere, in a layer known as the ionosphere. This layer ranges roughly from 85 to 110 km above Earth, and is so named because the gases there exist in ionic form. Rapidly moving particles from the sun can penetrate this layer, striking primarily oxygen and nitrogen atoms and causing them to radiate in the aurora's characteristic red or green colors. For a good site on aurora, visit http://logosphere@earthlink.net a> You might also be interested in visiting http:// members.mint.net/n1bug/prop/aumon/aufr.html which monitors aurora in real time. For great lightning pictures, my favorite site is the Australian Severe Weather Page, located at http:// australiansevereweather.simplenet.com/ and for an explanation and pictures of sprites and elves, go to http://www.sciam.com/explorations/012097sprites/ 012097explorations.html Happy skywatching!
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