Yu Mengying, Tan Yongbo, Shi Zheng, et al. Effects of channel-induced charge on discharge activity characteristics. J Appl Meteor Sci, 2019, 30(1): 105-116. DOI:  10.11898/1001-7313.20190110.
Citation: Yu Mengying, Tan Yongbo, Shi Zheng, et al. Effects of channel-induced charge on discharge activity characteristics. J Appl Meteor Sci, 2019, 30(1): 105-116. DOI:  10.11898/1001-7313.20190110.

Effects of Channel-induced Charge on Discharge Activity Characteristics

DOI: 10.11898/1001-7313.20190110
  • Received Date: 2018-08-02
  • Rev Recd Date: 2018-09-05
  • Publish Date: 2019-01-31
  • In order to explore effects of different polarity charge implantation method on the discharge of thunderstorm clouds in the charge-replacement scheme after lightning discharge, a batch of sensitive experiments are implemented by changing the channel-induced charge to simulate a typical thunderstorm case in Nanjing, based on existing three-dimensional (3-D) thunderstorm cloud electrification and discharge patterns. Eeffects of thunderstorm cloud discharge are discussed from the perspective of space charge structure after discharge, lightning channel length, lightning frequency and type. Simulations show that the amount of induced charge by the lightning channel has a significant effect on the spatial charge structure distribution and the length of the intra-cloud flash channel. As the amount of induced charge in the channel increases, the number of lattice points where the polarity of the space charge is reversed before and after discharge increases, and the space charge structure becomes more complex, which in turn increases the intra-cloud flash with a shorter length of the lightning channel. The space charge structure is disordered, and it becomes more difficult for a wide range of identical-polar charge stacks to form during the development process. Meanwhile, it is also difficult for the lightning channel to pass through charge stack with the same polarity during the propagation process, and therefore the intra-cloud flash channel is limited to a pair of smaller heteropolar charge stacks. Eventually, the frequency of intra-cloud flashes that leads to shorter lightning channel lengths increases. The total amount of channel induced charge accumulation under different induction control multiples can be considered approximately the same within the error tolerance. The frequency of intra-cloud flashes is negatively correlated with the average cumulative amount of channel charges in different lightning channel induced charges:When the average cumulative amount of channel induced charges increases, the frequency of intra-cloud flashes will decrease. The change of the induced charge amount in the channel makes the charge distribution of the space charge region unbalanced. The frequency and type of the cloud-to-ground flash are affected by many factors, and the changing pattern is not obvious. Therefore, the channel-induced charge amount has little correlation with the frequency and type of cloud-to-ground flashes.
  • Fig. 1  Environmental stratification curve(a) and vertical wind profile(b)

    Fig. 2  The variation trend of spatial charge polarity reversal lattice points with lightning order under different induction control multiples

    Fig. 3  Cross-section of the charge structure when t=21 min, y=42 km

    (isotherms of 0℃, -13.8℃, -40℃ are shown, thick black lines show the contour structure of the thundercloud)

    Fig. 4  The average cumulative amount of channel-induced charge, mean channel length, and lightning frequency change over time in the intra-cloud flash

    (a)the average cumulative amount of induced charges of the intra-cloud flash channel, (b)the average length of the intra-cloud flash channel, (c)the frequency of intra-cloud flash

    Fig. 5  Ratio of intra-cloud flash of channel lengths to total intra-cloud flash under different induction control multiples

    (a)channel lengths of the intra-cloud flash at 1-321 grid points, (b)channel lengths of the intra-cloud flash at 1-42 grid points

    Fig. 6  Trigger height of small channel length varying with time under different induction control multiples

    Fig. 7  Charge of the top shield, main positive and negative, and bottom positive charge in the early(a), mature(b), and dissipative(c) phases of thunderstorms at various induction control times

    Table  1  The average charge accumulation, intra-cloud flash frequency and channel induced charge accumulation under different induction control multiples

    感应控制倍数α 电荷平均累积量/C 云闪频次 通道感应电荷累积量/C
    0.3 6.73 1041 6684.5
    0.4 6.73 911 7454.1
    0.5 10.50 747 8355.5
    0.6 10.30 801 8320.1
    0.7 11.16 774 8644.9
    1 15.30 623 9567.9
    DownLoad: Download CSV

    Table  2  The total and the positive/negative ground flash frequency in different induction control multiples

    感应控制倍数α 总地闪频次 正地闪频次 负地闪频次
    0.3 194 58 136
    0.4 158 102 56
    0.5 139 93 46
    0.6 153 96 57
    0.7 160 47 113
    1 117 40 77
    DownLoad: Download CSV
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    • Received : 2018-08-02
    • Accepted : 2018-09-05
    • Published : 2019-01-31

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