Abstract
This work is devoted to a study of the conditions of initiation of two types of high-altitude discharges: sprites and halos. A quasi-electrostatic model of generation of the electric field in the middle atmosphere is developed; it takes into account the specific features of charge distribution and charge dynamics in the thundercloud, as well as real profile of the atmospheric conductivity. We take into consideration the nonlinear effects associated with the heating of electrons in the electric field. It is shown that the region where the electric field of the lightning flash exceeds the breakdown field is concentrated around an altitude of about 75 km, which is in agreement with the sprite observations. It is found that the dynamics of the current and discharge of the lightning flash plays a significant role in the initiation of high-altitude discharges in the atmosphere.
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References
E. R. Williams, “Sprites, Elves, and Flow Discharge Tubes,” Phys. Today 54, 41–47 (2001).
T. Neubert, “On Sprites and Their Exotic Kin,” Science 300, 747 (2003).
D. D. Sentman and E. M. Wescott, “Observations of Atmospheric Optical Flashes Recorded from an Aircraft,” Geophys. Rev. Lett. 20, 2857–2860 (1993).
E. A. Gerken, U. S. Inan, and C. P. Barrington-Leigh, “Telescoping Imaging of Sprites,” Geophys. Rev. Lett. 27(17), 2637–2640 (2000).
V. P. Pasko, U. S. Inan, and T. F. Bell, “Diffuse and Streamer Regions of Sprites,” Geophys. Rev. Lett. 29(10), 82–91 (2002).
V. P. Pasko, U. S. Inan, T. F. Bell, et al., “Sprites Produced by Quasi-Electrostatic Heating and Ionization in the Lower Ionosphere,” J. Geophys. Res. 102(A3), 4529–4561 (1997).
R. F. Fernsler and H. L. Rowland, “Models of Lightning-Produced Sprites and Elves,” J. Geophys. Res. 101(D23), 662 (1996).
E. R. Williams, E. Huang, R. Boldi, et al., “Criteria for Sprites and Elves Based on Schumann Resonance Observations,” J. Geophys. Res. 104(D14), 964 (1999).
E. I. Smirnova, E. A. Mareev, and Yu. V. Chugunov, “Modeling of Electric Field Transitional Processes,” Geophys. Rev. Lett. 27(23), 3833–3386 (2000).
V. A. Rakov and M. A. Uman, Lightning: Physics and Effects (Cambridge Univ. Press, Cambridge, 2002).
V. A. Rakov, R. Thottappillil, M. A. Uman, et al., “Mechanism of the Lightning M Component,” J. Geophys. Res. 100(D12), 25701–25710 (1995).
A. V. Gurevich and A. B. Shvartsburg, The Nonlinear Theory of the Propagation of Radio Waves in the Ionosphere (Nauka, Moscow, 1973) [in Russian].
V. L. Ginzburg, The Propagation of Electromagnetic Waves in Plasmas, 2nd ed. (Nauka, Moscow, 1967; Pergamon Press, Oxford, 1970).
N. D. Borisov, A. V. Gurevich, and G. M. Milikh, An Artificially Ionized Region in Atmosphere (IZMIRAN, Moscow, 1985) [in Russian].
R. H. Holzworth, M. C. Kelley, C. L. Siefring, et al., “Electrical Measurements in the Atmosphere and Ionosphere over an Active Thunderstorm: 2. Direct Current Electric Fields and Conductivity,” J. Geophys. Res. 90(A10), 9824–9830 (1985).
E. A. Mareev, A. A. Evtushenko, and S. A. Yashunin, Sprites, Elves, and Intense Lightning Discharges, Ed. by M. Fullekrug et al. (Springer, New York, 2006), pp. 313–340.
S. A. Yashunin, E. A. Mareev, and V. A. Rakov, “Are Lightning M Components Capable of Initiating Sprites and Sprite Halos?,” J. Geophys. Res. 112 D10109, doi: 10.1029/2006JD007631 (2007).
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Original Russian Text © E.A. Mareev, S.A. Yashunin, 2010, published in Izvestiya AN. Fizika Atmosfery i Okeana, 2010, Vol. 46, No. 1, pp. 78–84.
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Mareev, E.A., Yashunin, S.A. On conditions of initiation of electric discharges in the middle atmosphere. Izv. Atmos. Ocean. Phys. 46, 69–75 (2010). https://doi.org/10.1134/S000143381001010X
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DOI: https://doi.org/10.1134/S000143381001010X