From this web site:
http://www.albany.edu/faculty/rgk/atm101/sprite.htm
Red Sprites, Blue Jets and Elves
Red sprites, blue jets and elves are upper atmospheric optical phenomena associated with thunderstorms that have only recently been documented by using low light level television technology. These phenomena are collectively called Transient Luminous Events (TLE's)
Transient Luminous Events
Red sprites are large but weak luminous flashes that appear directly above an active thunderstorm system and are coincident with powerful positive cloud-to-ground lightning strokes. Their spatial structures range from small single or multiple vertically elongated spots, to bright groupings which extend from above the cloud tops to altitudes up to almost 60 miles (about 95 km. Sprites are predominantly red and they usually last no more than a few milliseconds. The brightest region lies in the altitude range 40 to 45 miles (about 65-75 km), above which there is often a faint red glow or wispy structure that extends to about 55 miles (90 km). Below the bright red region, blue tendril-like filamentary structures often extend downward to as low as 20 miles (30 km). Some events are loosely packed and may extend across horizontal distances of 30 miles (50 km) or more. Because of their low surface brightness, they have only been imaged at night (primarily with highly sensitive cameras). However, if ones eyes are sufficiently dark-adapted, one can actually detect them without any visual aid. The first images of a sprite were accidently obtained in 1989, although anecdotal reports of "rocket-like" and other optical emissions above thunderstorms go back more than a century. Early research reports for these events referred to them by a variety of names, including "upward lightning," "upward discharges," "cloud-to-stratosphere discharges," and "cloud-to-ionosphere discharges." Now they are simply referred to as sprites, a whimsical term that evokes a sense of their fleeting nature, while at the same time remaining nonjudgemental about physical processes that have yet to be determined.Blue jets are a second high altitude optical phenomenon, distinct from sprites and first documented in 1994 (although pilots had earlier reported similar sightings). Blue jets are optical ejections from the top of the electrically active core regions of thunderstorms, but not directly associated with cloud-to-ground lightning. Following their emergence from the top of the thundercloud, they typically propagate at about upward in narrow cones of about 15 degrees, fanning out and disappearing at heights of about 25-30 miles (40-50 km) with a lifetime of a couple of tenths of a second.
Elves are disk-shaped regions of luminosity, lasting less than a thousandth of a second, which occur high above energetic cloud-to-ground lightning of positive or negative polarity. Elves most likely result when an energetic electromagnetic pulse (EMP) propagates into the ionosphere. Though they can be accompanied by sprites, the causative mechanism is of an entirely different nature. Predicted to exist in the early 1990's and discovered in 1994, elves got their name as an acronym for Emission of Light and Very Low Frequency perturbations due to EMP Sources.
Sprite halos are even more recently discovered. They are diffuse disk shaped glows that apparently precede sprites and propagate downward from about 50 miles to 40 miles (85 to 70 km) altitude and last about a millisecond.
Trolls, also recently observed, resemble blue jets, but are red and seem to occur after tendrils of vigorous sprites extend downward toward the cloud tops.
Other emissions
There have recently been observed from space other types of unexpected non-luminous emissions that appear to originate from thunderstorms. These are:TIPPS (Trans-Ionospheric Pulse Pairs) are extremely intense pairs of VHF pulses originating from thunderstorm regions, but some 10,000 times stronger than sferics produced by normal lightning activity. They were first observed by the ALEXIS satellite.
Gamma ray bursts of short duration (about 1 millisecond) with terrestrial origin have been detected by the Compton Gamma Ray Observatory. They are observed to occur over thunderstorm regions, and their source is believed to lie at altitudes greater than 30 km.
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