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INTRICACIES OF LIGHTNING PART-1

机译:闪电第1部分的复杂性

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Lightning, the visible discharge of electricity that occurs when a region of a cloud acquires an excess electrical charge, either positive or negative, that is sufficient to break down the resistance of air. Lightning is a naturally occurring electrostatic discharge during which two electrically charged regions in the atmosphere or ground temporarily equalize themselves, causing the instantaneous release of as much as one gigajoule of energy. This discharge may produce a wide range of electromagnetic radiation, from very hot plasma created by the rapid movement of electrons to brilliant flashes of visible light in the form of black-body radiation. Lightning causes thunder, a sound from the shock wave that develops as gases in the vicinity of the discharge experience a sudden increase in pressure. Lightning occurs commonly during thunderstorms and other types of energetic weather systems, but volcanic lightning can also occur during volcanic eruptions.
机译:闪电,当云区域时,发生的电力的可见放电获取过量的电荷,正负的电荷或负,即足以分解空气的电阻。 闪电是一种天然存在的静电放电,在此期间,大气或地面中的两个电荷区域暂时均衡,导致瞬时释放多达一个千兆的能量。 这种放电可以产生各种电磁辐射,从通过电子的快速运动产生的非常热的等离子体以黑体辐射形式的可见光的辉煌闪烁。 闪电导致雷声,从放电附近的气体开发的冲击波的声音经历突然增加压力。 闪电通常发生在雷暴和其他类型的能量天气系统期间,但火山喷发过程中也可能发生火山闪电。

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  • 来源
    《Electrical India》 |2021年第8期|38-43|共6页
  • 作者

    Prabhat Khare;

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  • 正文语种 eng
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