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Determination of the Electric Field Intensity and Space Charge Density Versus Height Prior to Triggered Lightning

机译:触发雷电前电场强度和空间电荷密度与高度的确定

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摘要

We infer the vertical profiles of space charge density and electric field intensity above ground by comparing modeling and measurements of the ground-level electric field changes caused by elevating grounded lightning-triggering wires. The ground-level electric fields at distances of 60 m and 350 m were measured during six wire launches that resulted in triggered lightning. The wires were launched when ground-level electric fields ranged from 3.2 to 7.6 kV m−1 and the triggering heights ranged from 123 to 304 m. From wire launch time to lightning initiation time, the ground-level electric field reduction at 60 m ranged from 2.2 to 3.4 kV m−1, with little ground-level electric field reduction being observed at 350 m. We observed that the triggering heights were inversely proportional to the ground-level electric field when the wires were launched. Our Poisson equation solver simulates the ground-level electric field changes as the grounded wires extend in assumed vertically varying profiles of space charge density and electric field intensity. Our model reproduces the measured ground-level electric field changes when the assumed space charge density decays exponentially with altitude, with ground-level charge densities between 1.5 and 7 nC m−3, space charge exponential decay height constants ranging from 67 to 200 m, and uniform electric field intensities far above the space charge layer ranging from 20 to 60 kV m−1. Our model predicts typical charge densities on the wires of some tens of μC m−1 with milliampere-range currents flowing into the wires from ground to supply the wire charge.
机译:我们通过比较因高架接地的雷电触发导线引起的地平面电场变化的建模和测量结果,推断出地面上空间电荷密度和电场强度的垂直分布。在六次导线发射期间测量了距离为60 m和350 m的地面电场,该电场导致了雷击。当地面电场的范围为3.2到7.6 kV m-1,触发高度为123到304 m时,发射导线。从导线发射时间到雷电开始时间,在60 m处的地平面电场减小范围为2.2到3.4 kV m-1,在350 m处观察到的地平面电场减小很小。我们观察到,发射导线时,触发高度与地面电场成反比。我们的Poisson方程求解器模拟了接地线在假定的垂直方向上变化的空间电荷密度和电场强度分布情况下随着接地线的延伸而发生的变化。当假设的空间电荷密度随高度呈指数衰减时,我们的模型再现了测得的地面电场变化,其中地面电荷密度在1.5至7 nC m-3之间,空间电荷指数衰减高度常数范围为67至200 m,均匀的电场强度远远超过空间电荷层,范围从20到60 kV m-1。我们的模型预测了数十µC m-1的电线上的典型电荷密度,其中毫安范围的电流从地面流入电线以提供电线电荷。

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