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Upward leader inception caused by a sudden change of cloud electric field

机译:云电场突然变化引起的向上领导开始

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Discharge processes such as glow, streamer, and leader inception among others take place before an upward leader can be launched from a grounded structure during thunderstorms. Electrostatic fields below the thundercloud could lead to the formation of glow charge from grounded objects. if the electric field is high enough and ionization keeps expanding into the gap, streamers can be incepted. Depending on the available charge and the thermodynamic properties of the gas, there is a possibility to incept or not a positive upward leader towards the cloud. Usually, the inception of positive upward leaders is directly related with the appearance of a downward coming leader from cloud towards the grounded object. Such a downward leader will intensify the electric field in such a way that the streamer discharges could thermalize and produce an unstable upward leader channel. However, experimental observations have indicated the inception of upward leaders from grounded structures without registering connecting downward leaders towards the structure. The present paper intends to explain the inception of positive upward leaders from the top of a rod, whenever the electric field produced by the cloud suddenly changes e.g. due to intra-cloud discharges or distance cloud to ground flash. A two dimensional model based on the gas-dynamic equations, the main processes responsible for gas heating such as vibrational excitation and transfer of energy into electronic, rotational and translational excitation, coupled with Poisson equation is presented in this paper. Rods of different lengths under thundercloud electric field were studied. Simulation results indicate that positive upward leaders can be incepted from long rods under certain conditions of thundercloud electric field without the need of a coming downward leader. However, for rods of tenths of meters the thundercloud electric field is not enough to incept positive upward leaders and an intensification of the electric fiel- is required in order to incept a positive upward leader from the structure, e.g., a coming downward leader.
机译:在雷暴天气中,要先从地面结构发射向上的领导者,然后进行辉光,流光和领导者起始等放电过程。雷云下方的静电场可能导致接地物体产生辉光电荷。如果电场足够高并且电离持续扩展到间隙中,则可以看到流光。根据可用的电荷和气体的热力学性质,是否有可能接受或不向云层积极向上引导。通常,积极向上的领导者的出现与从云层向下朝着地面物体的向下走向的领导者的出现直接相关。这样的向下引导器将以如下方式增强电场,使得拖缆放电会热化并产生不稳定的向上引导器通道。但是,实验观察表明,从接地结构开始出现向上的引导器,而没有记录将向下的引导器连接到结构。本文旨在解释无论何时由云产生的电场突然改变(例如),从杆的顶部开始出现积极向上的引导者。由于云内放电或云层与地面的距离较远。提出了一种基于气体动力学方程的二维模型,结合了泊松方程,该模型是负责气体加热的主要过程,如振动激发以及将能量转换为电子,旋转和平移激发的过程。研究了雷云电场作用下不同长度的棒。仿真结果表明,在一定的雷云电场条件下,长杆可以接收到正的向上引导,而无需向下的引导。然而,对于十分之一米的杆,雷云电场不足以接受正向引导,因此需要加强电场以从结构中接受正向引导,例如向下的引导。

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