Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component in thunder-storm charging and discharging processes (e.g., Loeb,1965; MacGorman and Rust,1998; Rakov andUman,2003). Many studies have been conducted to investigate the onset condition and the characteristics of corona discharges from water drops and ice particles. 19 Septem ber,2009 60940 60960 60980 61000 61020 61040 61060 61080 21:07:12 21:36:00 22:04:48 22:33:36 23:02:24 23:31:12 0:00:00 UT Pressure 39500 40000 40500 41000 41500 42000 42500 Count rate Aragats pressure ArNM 4 O ctober,2010 61360 61370 61380 61390 61400 61410 61420 61430 61440 16:19:12 16:48:00 17:16:48 17:45:36 18:14:24 18:43:12 19:12:00 UT Pressure 37000 37500 38000 38500 39000 39500 40000 40500 41000 Count rate Aragats P ressure ArNM
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Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component.
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Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul
Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component in thunder-storm charging and discharging processes (e.g., Loeb,1965; MacGorman and Rust,1998; Rakov andUman,2003). Many studies
have been conducted to investigate the onset condition and the characteristics of corona discharges from water drops and ice particles.