Abstract
Red sprites, different from lightning flashes occurring in the troposphere, are large and brief discharges which appear in the altitude range from about 40 to 90 km above large thunderstorms and are usually caused by cloud-to-ground lightning discharges (CGs). A total of 17 sprites over two thunderstorms were first observed during the summer of 2007. One of the sprites occurred on July 28 above a thunderstorm in Guan County and the center of the storm was about 272 km from the observation site. The other sprites were recorded at the late night of August 1 and in the early morning of August 2, and the storm center was about 315 km away. All of the observed sprites occurred in cluster, and their appearances were very different, including ‘columniform sprites’, ‘columniform sprites’ with angel-like wings, ‘carrot sprites’, ‘dancing sprites’, etc. The duration of the sprites varied from a minimum of 40 ms to a maximum of 160 ms with a geometric mean (GM) of 61 ms. The time delay between parental positive cloud-to-ground lightning flashes (+CGs) and the associated sprites varied from 3.4 to 11.8 ms with a GM of 7.1 ms. The ratio of the number of +CGs to the total number of CGs during the time period with sprites was 7 times larger than that when no sprites occurred. Sprites did not appear frequently at the time when the convective activity is strong but when the thunderstorm starts to become weak.
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References
Franz R C, Nemzek R J, Winckler J R. Television image of a large upward electrical discharge above a thunderstorm system. Science, 1990, 249(4964):48–51
Lyons W A. Characteristics of luminous structures in the stratosphere above thunderstorms as imaged by low-light video. Geophys Res Lett, 1994, 21(10):875–878
Sentman D D, Wescott E M, Osborne D L, et al. Preliminary results from Sprites94 campaign: 1.Red sprites. Geophys Res Lett, 1995, 22(10):1205–1208
Westcott E M, Sentman D D, Osborne D L, et al. Preliminary resuts from the Sprites94 aircraft campaitn: 2. Blue jets. Geophys Res Lett, 1995, 22(10):1209–1212
Pasko V P, Stanley M A, Mathews J D, et a1. Electrical discharge from a thundercloud top to the lower ionosphere. Nature, 2002, 416(6877):152–154
Wescott E M, Sentman D D, Heavner M J, et al. Observations of ‘Columniform’ sprites.J Atmos Sol Terr Phys, 1998, 60(7–9):733–740
Su H t, Hsu R R, Chen A B, et al. Observation of sprites over the Asian continent and over oceans around Taiwan. Geophys Res Lett, 2002, 29(4), doi:10.1029/2001GL013737
Zhu B Y, Tao S C, Tan Y B. Review of high-altitude air discharges above thunderstorms. Plateau Meteorol, 2006, 25(3):549–555
Wu M L, Xu J Y. A time-dependent quasi-three-dimensional QEF model of red sprites. Chinese J Geophys, 2005, 48(3):480–486
Wu M L, Xu J Y, Ma R P. The simulation study of spherics and red sprite phenomena produced by lightning. Acta Phys Sin, 2006, 55(10):5007–5013
Wu M L, Xu J Y. Time-dependent simulation of electric field configuration and optical emission of sprite halo. Chin J Space Sci, 2005, 25(6):510–515
Winckler J R. Further observations of cloud-ionosphere electrical discharges above thunderstorms. J Geophys Res, 1995, 100(D7):14335–14345
Fernanda T, Sabbas S, Sentman D D, et al. Statistical analysis of space-time relationships between sprites and lightning. J Atmos Solar Terr Phys, 2003, 65(5):525–535
Hsu R R, Su H T, Chen A B, et al. Transient luminous events in the vicinity of Taiwan. J Atmos Solar Terr Phys, 2003, 65(5):561–566
Pasko V P, Inan U S, Bell T F, et al. Sprites produced by quasi-electrostatic heating and ionization in the lower ionosphere. J Geophys Res, 1997, 102(A3):4529–4561
Winckler J R. Optical and VLF radio observations of sprites over a frontal storm viewed from O’Brien Observatory of the University of Minnesota. J Atmos Solar Terr Phys, 1998, 60(7–9):679–688
Price C, Yair Y, Asfur M. East African lightning as a precursor of Atlantic hurricane activity. Geophys Res Lett, 2007, 34(L09805), doi:10.1029/2006GL028884
Lyons W A. Sprite observations above the U.S. High Plains in relation to their parent thunderstorm systems. J Geophys Res, 1996, 101(23):29641–29652
Valdivia J A, Milikh G, Papadopoulos K. Red sprites: Lightning as a fractal antenna. Geophys Res Lett, 1997, 24(24):3169–3172
Suzuki T, Hayakawa M, Matsudo Y, et al. How do winter thunderstorm systems generate sprite-inducing lightning in the Hokuriku area of Japan? Geophys Res Lett, 2006, 33, L10806, doi:10.1029/2005GL025433
Ganot M, Yair Y, Price C, et al. First detection of transient luminous events associated with winter thunderstorms in the eastern Mediterranean. Geophys Res Lett, 2007, 34, L12801, doi:10.1029/2007GL029258
Pinto O J, Saba M M F, Pinto R C A, et al. Thunderstorm and lightning characteristics associated with sprites in Brazil. Geophys Res Lett, 2004, 31, L13103, doi:10.1029/2004GL020264
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Supported by the Main Direction Program of the Knowledge Innovation of Chinese Academy of Sciences (Grant No. KZCX2-YW-206), the National Natural Science Foundation for Distinguished Young Scholars of China (Grant No. 40325013) and the National Natural Science Foundation of China (Grant No. 40774083)
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Jing, Y., XiuShu, Q., GuangShu, Z. et al. Red sprites over thunderstorms in the coast of Shandong Province, China. Chin. Sci. Bull. 53, 1079–1086 (2008). https://doi.org/10.1007/s11434-008-0141-8
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DOI: https://doi.org/10.1007/s11434-008-0141-8