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Fine-resolution Simulation Of Cloud-to-ground Lightning And Thundercloud Charge Transfer

机译:云对地闪电和雷云电荷转移的精细模拟

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摘要

2-D 12.5 m-resolution simulations of cloud-to-ground (CG) lightning discharge processes have been performed using an improved stochastic lightning model for different types of cloud charge distributions, such as dipole, tripole, bi-dipole and multi-layer charge structures produced from the numerical simulation of thundercloud electrification. The modelling produced the fine branched channel structure of CG lightning and the results illustrate the relations between CG lightning channel propagation and cloud charge distribution. The simulated features of CG lightning are associated with the observed results. The simulation studies are essential in our understanding of complex charge transfer processes caused by CG lightning discharges in thunderclouds. The induced charges of opposite polarity are deposited or embedded in the local volumes where the bidirectional leaders passed during a CG lightning discharge. Although the embedding affects charge structure only in a pair of significant positive and negative charge regions closest to the ground, the electric field strength acutely weakens and electrostatic energy in thunderclouds is significantly consumed when the discharge terminates. In addition to simulating the upward and downward breakdown of the initial leader to ground and the ensuing return stroke (RS), the simulation assumes that current continues to flow in the channel to ground and determines the upward breakdown until the end of the discharge. For the subsequent discharge sub-process, the upward leader channel tends to transfer the charges with the same polarity as the RS, while the downward leader channel favors transfer of opposite charge to ground. In the sub-processes of a few CG flash simulations, the magnitude of the opposite charges from the downward leader exceeds that of charges with the same polarity from the upward leader so that the net charges transferred to the ground have a reversed polarity to the RS. The simulation presents similar features of CG lightning as those observed in realistic bipolar CG lightning.
机译:使用改进的随机闪电模型针对不同类型的云电荷分布(如偶极子,三极子,双偶极子和多层)进行了2-D 12.5 m分辨率的云对地(CG)闪电放电过程模拟雷云电气化数值模拟产生的电荷结构。该模型产生了CG闪电的精细分支通道结构,结果说明了CG闪电通道传播与云电荷分布之间的关系。 CG闪电的模拟特征与观测结果相关。对于理解由雷云中CG闪电放电引起的复杂电荷转移过程而言,模拟研究至关重要。极性相反的感应电荷沉积或嵌入CG闪电放电期间双向引导器通过的局部体积中。尽管嵌入仅在最接近地面的一对显着的正负电荷区域中影响电荷结构,但是当放电终止时,电场强度会急剧减弱,雷云中的静电能量会被大量消耗。除了模拟初始引导线对地面的向上和向下击穿以及随之而来的回程(RS),该模拟还假设电流继续在通道中流向地面,并确定向上的击穿直到放电结束。对于随后的放电子过程,向上的引导通道倾向于以与RS相同的极性转移电荷,而向下的引导通道则倾向于将相反的电荷转移到地面。在一些CG闪存模拟的子过程中,来自向下引导器的相反电荷的大小超过了来自向上引导器的具有相同极性的电荷的大小,因此传输到地面的净电荷与RS具有相反的极性。该仿真呈现的CG闪电与实际双极CG闪电中观察到的特征相似。

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