Numerical simulations of the bi-level and branched structure of intracloud lightning flashes

被引:1
作者
Yongbo Tan
Shanchang Tao
Baoyou Zhu
Ming Ma
Weitao Lu
机构
[1] University of Science and Technology of China,School of Earth and Space Sciences
[2] Chinese Academy of Meteorological Sciences,undefined
来源
Science in China Series D | 2006年 / 49卷
关键词
IC; lightning parameterization; branched bilevel structure; fractal feature; propagation tendency;
D O I
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中图分类号
学科分类号
摘要
Intracloud (IC) lightning flashes have been simulated in fine resolution (12.5 m) by using a bidirectional stochastic lightning parameterization scheme within 2-dimensional domain. The simulated results show that the IC flashes have a bilevel channel structure and the altitudes of the horizontal channels are at the same heights of potential wells, which are supported by the previous VHF source observations and balloon soundings of electric field profile in the thundercloud. Further conclusions are: (1) After an IC flash is initiated near the boundary between positve and nagetive charge zone, the negative (or positive) leader tends to propagate into the positive (or negative) charge zone. Both types of positive and negative IC flashes have been reproduced and their polarity depends on the up and down disposition of the positive and negative charge regions. (2) The extension range of leaders is correlative with the cloud charge distribution. The leader is possible to extend through the inverted charge region all over where it is extending, but keeps away from the isolated charge area of the same polarity. (3) The channel structures also depend on the electric potential distributions in the thundercloud. Before propagating into the central area of potential wells, the leader tends to extend along the direction with the maximum of potential gradient. Once extending away from the center of potential wells, the leader tends to extend along the direction with the slowest potential change. (4) The IC flash channels have the fractal feature with fractal dimension 1.45 before leaders pass through the central area of charge regions. The exponent decreases rapidly once leaders extend into the low-density charge regions. (5) The induced charges of opposite polarity are deposited in the leader channels within preexisting positive and negative charge regions during IC flash discharges. This causes a new and complicated charge distribution in the thundercloud, and the potential extremum drops from 200 to 20 Mv when the IC flash terminates.
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页码:661 / 672
页数:11
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