Abstract. A balloon-borne instrument was designed to measure the electric field in
thunderstorms. One case of thunderstorm was observed in the Pingliang region
(35.57∘ N, 106.59∘ E; and 1620 m above sea level, a.s.l.)
of a Chinese inland plateau, through penetration by the balloon-borne
sounding in the early period of the mature stage. Results showed that the
sounding passed through seven predominant charge regions. A negative charge
region with a depth of 800 m located near the surface, and a positive charge
region appeared in the warm cloud region; their mean charge densities were
−0.44 ± 0.136 and 0.43 ± 0.103 nC m−3, respectively.
Five charge regions existed in the region colder than 0 ∘C, and
charge polarity alternated in a vertical direction with a positive charge at
the lowest region. The mean charge densities for these five regions were
0.40±0.037 nC m−3 (−9.5 to −4 ∘C), -0.63±0.0107 nC m−3 (−18 to −14 ∘C), 0.35±0.063 nC m−3 (−27 to −18 ∘C), -0.36±0.057 nC m−3 (−34 to −27 ∘C), and 0.24±0.06 nC m−3 (−38 to −34 ∘C). We speculated that the two
independent positive charge regions in the lower portion are the same charge
region with a weak charge density layer in the middle. The analysis showed
that the real charge structure of the thunderstorm is more complex than the
tripole model, and the lower dipole is the most intensive charge region in
the thunderstorm. Keywords. Meteorology and atmospheric dynamics (atmospheric electricity)
Measurements of vertical electric field in a thunderstorm in a Chinese inland plateau