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Historically, the process of transient luminous event (TLE) detection has required an alert human observer on a low light level television (LLTV) monitor, either in real time or playback.
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On timescales measured in fractions of a second, high-speed cameras can record luminous events in the flash.
In addition, electrical discharges from the tops of thunderstorms into the ionosphere, called transient luminous events, have been observed.
First discovered in the 1960s, these powerfully luminous events long remained completely mysterious, since there seemed no evidence of their sources at visible or radio wavelengths.
The scientific goals of this mission are to investigate lightning-induced transient luminous events (TLEs), polar aurora, and upper atmospheric airglow.
The JEM-GLIMS mission aims to observe global distributions of lightning and lightning-associated transient luminous events (TLEs) by combining observations with radio and optical sensors.
The JEM-GLIMS mission is designed to conduct comprehensive observations with both EM and optical payloads for lightning activities and related transient luminous events.
In total numbers, the number of −CG transient luminous events (TLEs) (presumably all halos) predominates over the number of +CG TLEs.
The purpose of this paper is to summarize the enormous contributions of FS2 (FORMOSAT-2 or Formosa satellite #2) in both Earth and transient luminous events (TLEs) observations in 10 years.
Rates of detection were simulated for two different systems: the SPOSH (Smart Panoramic Optical Sensor Head) camera optimized for the observation of transient luminous events, and the JEM-EUSO (Japanese Experiment Module-Extreme Universe Space Observatory) experiment on the ISS International Space Stationn).
Three axis electric and magnetic field and ground-based low light level TV observations from three sites were made of more than 68 transient luminous events (TLEs) in the middle atmosphere above thunderstorms in South Dakota and Kansas.
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