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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >DISTRIBUTION OF CHARGE ALONG THE LIGHTNING CHANNEL - RELATION TO REMOTE ELECTRIC AND MAGNETIC FIELDS AND TO RETURN-STROKE MODELS
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DISTRIBUTION OF CHARGE ALONG THE LIGHTNING CHANNEL - RELATION TO REMOTE ELECTRIC AND MAGNETIC FIELDS AND TO RETURN-STROKE MODELS

机译:闪电通道上电荷的分布-与远程电场和磁场以及与反冲模型的关系。

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摘要

We derive exact expressions for remote electric and magnetic fields as a function of the time- and height-varying charge density on the lightning channel for both leader and return-stroke processes. Further, we determine the charge density distributions for six return-stroke models. The charge density during the return-stroke process is expressed as the sum of two components, one component being associated with the return-stroke charge transferred through a given channel section and the other component with the charge deposited by the return stroke on this channel section. After the return-stroke process has been completed, the total charge density on the channel is equal to the deposited charge density component. The charge density distribution along the channel corresponding to the original transmission line (TL) model has only a transferred charge density component so that the charge density is everywhere zero after the wave has traversed the channel. For the Bruce-Golde (BG) model there is no transferred, only a deposited, charge density component. The total charge density distribution for the version of the modified transmission line model that is characterized by an exponential current decay with height (MTLE) is unrealistically skewed toward the bottom of the channel, as evidenced by field calculations using this distribution that yield (1) a large electric field ramp at ranges of the order of some tens of meters not observed in the measured electric fields from triggered-lightning return strokes and (2) a ratio of leader-to-return-stroke electric field at far distances that is about 3 times larger than typically observed. The BG model, the traveling current source (TCS) model, the version of the modified transmission line model that is characterized by a linear current decay with height (MTLL), and the Diendorfer-Uman (DU) model appear to be consistent with the available experimental data on very close electric fields from triggered-lightning return strokes and predict a distant leader-to-return-stroke electric field ratio not far from unity, in keeping with the observations. In the TCS and DU models the distribution of total charge density along the channel during the return-stroke process is influenced by the inherent assumption that the current reflection coefficient at ground is equal to zero, the latter condition being invalid for the case of a lightning strike to a well-grounded object where an appreciable reflection is expected from ground. [References: 21]
机译:我们得出远距离电场和磁场的精确表达式,作为前导和返回冲程过程中雷电通道上随时间和高度变化的电荷密度的函数。此外,我们确定了六个返回冲程模型的电荷密度分布。在返回冲程过程中的电荷密度表示为两个分量的总和,一个分量与通过给定通道部分传输的返回冲程电荷相关联,另一个分量与返回冲程在该通道部分上沉积的电荷相关联。回程过程完成后,通道上的总电荷密度等于沉积的电荷密度分量。沿着与原始传输线(TL)模型相对应的通道的电荷密度分布仅具有转移的电荷密度分量,因此在波经过通道之后,电荷密度在各处都为零。对于Bruce-Golde(BG)模型,没有转移,只有沉积的电荷密度成分。修改后的传输线模型版本的总电荷密度分布以高度随时间变化的指数电流衰减(MTLE)为特征,这不切实际地偏向通道底部,这一点通过使用这种分布产生的场计算得到证明(1)从触发的雷击回程在测得的电场中未观察到数十米范围内的大电场斜率,并且(2)在远距离处的先导与回击电场之比约为比通常观察到的大3倍。 BG模型,行进电流源(TCS)模型,以高度随时间变化的线性电流(MTLL)为特征的改进型传输线模型以及Diendorfer-Uman(DU)模型似乎与与触发雷击的非常近的电场相关的可用实验数据,并根据观察结果预测了不远的统一的首长与重击的电场比。在TCS和DU模型中,回击过程中沿通道的总电荷密度分布受以下固有假设影响:地面的电流反射系数等于零,对于闪电情况,后一种情况无效撞击到接地良好的物体,预计会从地面反射出明显的反射。 [参考:21]

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