By R. Ghahawala
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Geophys. Res. 19, (January 1, 1992), pp. 1029/91GL03168. Boeck, W. , et al. (1995). Observations of lightning in the stratosphere. J. Geophys. 100, (January 1, 1995), pp. 1029/94JD02432. Boeck, W. , et al. (1998). The role of the space shuttle videotapes in the discovery of sprites, jets and elves. J. Atmos. Sol. Terr. 60, (May 1, 1998), pp. 1016/S1364-6826(98)00025-X. , & Solomon, S. (1986). Aeronomy of the middle atmosphere : chemistry and physics of the stratosphere and mesosphere (2nd), D. Reidel Pub.
2007). In the high tail of electron energy distribution, runaway electron may be up to several kilo electron volt of electron energy. Besides, these energetic electron avalanches in gas breakdown may cause the plasma erosion on the heat shield of space shuttle. Therefore, it is necessary to have space missions to investigate the possible damages on re-entry of space shuttle. 7. Conclusion Discharge phenomena in the middle atmosphere are one of the hottest research fields for satellite missions; currently with the ISUAL, the Tatiana-2, the SPRITE-SAT, Chibis-M missions perform daily observations of TLEs from space.
Sprite spectra; N2 1 PG band identification. Geophys. Res. 22, (n/a 1, 1995), pp. 1029/95GL02827. Mende, S. , et al. (2005). D region ionization by lightning-induced electromagnetic pulses. J. Geophys. 110, (November 1, 2005), pp. 1029/2005JA011064. ; Valdivia, J. , & Papadopoulos, K. (1998). Spectrum of red sprites. J. Atmos. Sol. Terr. 60, (May 1, 1998), pp. 1016/S1364-6826(98)00032-7. Morgan, W. , & Penetrante, B. M. (1990). ELENDIF: A time-dependent Boltzmann solver for partially ionized plasmas.