![]() ![]() ![]() Finally, a need for observation aimed data accumulation and further theoretical study of TLEs were identified, and some presently unsolved problems in the theory of TLEs were outlined. The effects of TLEs on the stratosphere, mesosphere and ionosphere were discussed. The image was obtained at 05:24:22. An attempt was made to summarize the general phenomenology on morphological features of TLEs based on the available experimental data and the interpretation of these observed features with modeling efforts. Cover Image: A massive transient luminous event termed sprite observed at mesospheric altitudes above a lightning producing Nebraska thunderstorm. Because the operational methodology was planned. The known TLEs can be classified into four categories, Red Sprites that develop at the base of the ionosphere and move rapidly downward Blue Jets, which emanate from the top of thunderclouds up to an altitude of 40 km ELVEs, which occurred in the lower ionosphere region and can spread over 300 km laterally and upward moving Gigantic Jets, which establish a direct path of electrical connection between thundercloud tops and the lower ionosphere. Mesoscale convective systems offer a high probability for the occurrence of TLEs above active thunderstorms. Theres another world of weird, ghostly lights that most humans never see, dancing. Abstract An overview of general phenomenology and proposed physical mechanisms of large scale electrical discharges termed blue jets and gigantic jets observed at high altitude in the Earths atmosphere above thunderstorms is presented. ( 1990) serendipitously during a test of a low-light television camera. Transient Luminous Events Lightning isnt the only electrical trickery thunderstorms have up their sleeves. Transient luminous events (TLEs) are large scale optical events occurring at high altitudes, which are related to the electrical activity in underlying thunderstorms. Special credit has been paid in the past to the study of transient luminous events (TLEs) that occasionally occur above a large thunderstorm at stratospheric and mesospheric altitudes. ![]()
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