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Post Info TOPIC: Transient luminous events


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Elves and sprites
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Storm elves and sprites recorded on video

A team of Spanish researchers has made a high-speed recording of elves and sprites in storms, fleeting and luminous electric phenomena produced in the upper layers of the atmosphere. Their analysis of these observations has been published in the Journal of Geophysical Research.

"This is the first time in Europe that we have been able to use high-speed video to detect transitory luminous phenomena taking place in the upper atmosphere - so-called sprites (in the form of a carrot or column) and elves (which are ring shaped)" - Joan Montanyà, co-author of the study and a researcher at the Department of Electric Energy at the Polytechnic University of Catalonia (UPC), tells SINC.

The results have been published in the Journal of Geophysical Research and show there are many fewer elves in storms that form over land than those at sea, where electric currents apparently have greater energy, especially in winter. Some of the recordings show elves and sprites at the same time, evidence of the strength of lightning over the sea during winter storms.
The scientists also observed the interaction between two sprites. A branch of one of them hit and bounced off the second, giving clues about their dynamics and electric structure. Sprites normally appear for around 40 milliseconds and 20 or 30 kilometres away from the site of the lightning.


Graban en vídeo a los duendes y elfos de las tormentas

Un equipo de investigadores españoles ha grabado por primera vez en Europa a alta velocidad a los duendes y elfos de las tormentas, unos fenómenos eléctricos fugaces y luminosos que se producen en las capas altas de la atmósfera. El análisis de las observaciones se ha publicado en el Journal of Geophysical Research.
Read more (Spanish)

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L

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Sprites
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Tel Aviv University leads global studies of "sprites," a natural phenomenon related to thunderstorms
In legend, sprites are trolls, elves and other spirits that dance high above our ozone layer. But scientists at Tel Aviv University have discovered that some very real "sprites" are zipping across the atmosphere as well, providing a possible explanation for those other legendary denizens of the skies, UFOs.
Thunderstorms, says Prof. Colin Price, head of the Geophysics and Planetary Sciences Department at Tel Aviv University, are the catalyst for a newly discovered natural phenomenon he calls "sprites." He and his colleagues are one of the leading teams in the world studying the phenomenon, and Prof. Price leads the study of "winter sprites" - those that appear only in the northern hemisphere's winter months.

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 Blink during a thunderstorm and you may miss the unusual phenomenon of "sprites"resplendent bursts of light that, for less than a second, burn brighter than Venus.
These brief explosions, which can outshine everything except for the sun and moon, are so fleeting, that scientists still don't know much about how they work.
So in a recent study, a group of physicists used an ultra high-speed digital camera to record sprites in unprecedented detail10,000 frames per second.

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Researchers at Duke University’s Pratt School of Engineering have captured the best images ever produced of "sprites" -- mysterious flashes of light resembling giant undulating jellyfish that can occur above strong thunderstorms -- using a high-speed camera that recorded thousands of video frames a second.

The researchers said their findings could lead to a better understanding of the physics and chemistry of this fleeting, still-unexplained lightning phenomenon. They recorded and analysed video of sprites associated with powerful thunderstorms occurring over the Great Plains during the summer of 2005. Their findings are scheduled to appear online in Geophysical Research Letters on February 22. The research was supported by the National Science Foundation.

"By analysing the high-speed images in sequence, we’ve been able to clearly define, for the first time, the processes by which sprites develop and what happens inside of them. This understanding of sprite structure is a necessary step to further elucidate sprite dynamics and their possible effects on the upper atmosphere" - Steven Cummer, assistant professor of electrical and computer engineering at Duke’s Pratt School.



Sprites are one of the most common of a number of so-called mesospheric transient luminous events (TLEs) driven by lightning. Other such lightning-related phenomena include blue jets, elves and terrestrial gamma ray flashes.
Since sprites were discovered in 1989, scientists have been attempting to measure and document them. The first high-speed images of sprites were reported by other researchers in 1999. Shortly thereafter, a second group captured the first images of sprites recorded at 1,000 frames per second.

"Each improvement has revealed important new information about the processes involved and their possible larger scale impact on the upper atmosphere. However, many sprites develop too quickly to be fully resolved even at one millisecond time resolution" - Steven Cummer.

Sprites typically last for 10 to 100 milliseconds -- shorter than the blink of a human eye, which takes an average of 300 to 400 milliseconds. Their transience makes sprites difficult to see with the naked eye, despite their common occurrence in association with certain types of active thunderstorms, the researchers said.
The vantagepoint required for a good view also complicates direct observation of sprites. Sprites generally form between 20 and 50 miles above storms and can often be obscured by lower lying thunderclouds. Therefore, it’s best to view them from a mountaintop or other high point about 100 to 300 miles away from a storm.
The Pratt team -- along with collaborators Walter Lyons and Thomas Nelson of FMA Research Inc. in Fort Collins, Colorado – set up an intensified high-speed camera capable of recording more than 5,000 frames per second at the Yucca Ridge Field Station in Fort Collins from July through August 2005. From that site, the researchers could look out over the Great Plains to image storms occurring over Kansas and Nebraska.
Night after night, the group watched the weather forecast for conditions ripe for sprites. When a promising storm was brewing, the researchers pointed the high- speed camera in the right direction and watched events unfold remotely on a television displaying video from a low-light camera.

"Sometimes we’d get lucky and there would be a sprite every 10 to 15 minutes. Other times, we would wait for four hours and only get two events" - Nicolas Jaugey, a member of Cummer’s team at the Pratt School.

Although much of the time was spent waiting, the researchers had to keep a very close watch in order to capture the sprites. The events happen so fast that they would often occur in just one normal speed video frame.

"They happen about as fast as you can possibly see anything on a normal television We had to watch for brief flashes and call them out when they happened" - Nicolas Jaugey.

This meant that the team had to be particularly adept at differentiating flashes indicative of a sprite from lightning itself.
When the proper type of flash was seen, one of the team members pressed a button to start the high-speed camera recording. The cameras record so much data so quickly that they can only be activated when a suspected sprite occurs.

"When we knew a storm was good, it wasn’t a problem to wait. When a sprite is captured on film, it’s extremely exciting. You see just a flash on the TV screen, but when you retrieve the recording from the high-speed camera and see its development, it’s very beautiful" - Nicolas Jaugey

Over the entire field season, the researchers captured 76 TLE sequences on seven different nights, 66 of which contained distinguishable sprite elements, they reported. As luck would have it, they produced the best images on the night of August 13 -- their very last day in the field. It is those images that the team analysed in detail in the latest report.
Based on the observations, sprites normally begin almost 50 miles high as downward-moving “streamers” that appear spontaneously or at the bottom of a halo -- diffuse flashes of light often associated with sprites. The streamers then branch out as they move down. At the same time, a brighter column of light expands both up and down from the starting point, followed by bright streamers that shoot higher into the sky.
The group’s videos also revealed new details of “isolated dots,” bright spots of light -- first described by other investigators -- that often glow for longer than any other portion of the sprite. The pictures show that some of these bright spots form when individual streamers collide, presumably as a result of electrostatic attraction between them.
The greater energy intensity found at those spots makes them particularly important for understanding the impact of sprites on atmospheric chemistry.

"Electrons with enough energy to produce light can also produce interesting chemical species not normally generated. Such chemicals might be long-lived and could be transported to other locations through the atmosphere" - Steven Cummer.

Because isolated dots persist for the longest, they may be sites where a significant portion of such chemical reactions occur.
The new insight into how these bright spots form could lead other researchers to produce better models of their physics and chemistry, he said. The Duke team will also conduct further analyses to relate their sprite image sequences to information they gathered on the lightning-produced magnetic and electric fields that spawned them.

"We should be able to make new connections between the lightning strength and speed required to produce these phenomena in the upper atmosphere" - Steven Cummer.

Other collaborators on the study included Jingbo Li, of Duke, and Elizabeth Gerken, of SRI International in Menlo Park, California.

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Transient luminous events
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Do giant flashes of lightning striking upwards from thunder clouds merely pose an extraordinarily spectacular view?
Or do they actually alter the chemical composition of the atmosphere, playing a role in ozone depletion and the climate on Earth?
This is the key question that may be answered by specially designed cameras, which ESA proposes to place on board the International Space Station.

The International Space Station (ISS) is the ideal setting for studies of spectacular natural phenomena well hidden from us on Earth - so-called red sprites, blue jets and elves: vast flashes of lightning striking not from clouds to the ground, but from clouds towards space.



Red sprites, blue jets, elves and sprite halos, collectively termed "transient luminous events" are caused by the discharge of lightning from storm clouds into the upper atmosphere and ionosphere, which begins at an altitude of about 100 kilometres.
These discharges produce much different effects from the craggy lightning discharges to the ground. But little is known about them because they occur between 50 and 100 kilometres above the earth's surface, too high for airplanes to study and too low for most satellites.

Normally the word lightning makes us think of sharp zigzag lines striking from the clouds to the ground. Above the clouds however a quite different type of lightning can be seen. There lightning is colourful - mainly red and blue - and covers large areas of the upper atmosphere. Sometimes it can even reach the border between the atmosphere and space.

Over the last few years scientists from the Danish National Space Centre have studied these flashes with cameras placed on mountain tops. Every so often the cameras would catch a flash of lightning striking up from a thunder cloud at a lower altitude.

Placing cameras and other instruments on the Space Station would, however, dramatically improve the chances of seeing the giant flashes and study their effect on the atmosphere. The Danish National Space Centre is currently studying a package of instruments for just that purpose, known as the Atmosphere-Space Interactions Monitor (ASIM).
ESA has now selected ASIM for a feasibility study (known as Phase A).


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"The question is how are these giant flashes of lightning created and how often do they take place" - Torben Neubert, senior scientist, head of the project at Danish National Space Centre.

It may well be that the large electrical bursts remove ozone from the atmosphere, and in so doing influence the climate.

"We need to understand the natural processes which influence the atmosphere and this can help us decide which changes in the climate are man-made" - Torben Neubert.

It is still too early to say when the cameras will actually enter into service in space.

Source: ESA

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