Lightning

Models for the charge buildup which leads to lightning discharges suggest a buildup of a strong negative charge layer near the bottom of the cloud and the formation of a positive ground shadow. When the buildup is large enough to produce ionization of the air, a lightning discharge is initiated. This is called the positive dipole structure for the charge buildup. More recent studies indicate a tripolar structure. 关于导致雷电放电的电荷积累模型表明，云层底部附近会形成一个强负电荷层，并产生一个正的地面影子。当电荷积累足够大，引起空气离子化时，就会发生雷电放电。这种现象被称为正双极结构。更近期的研究表明，这实际上是一个三极结构。 With voltages of hundreds of millions of volts and currents in the tens of thousands of amperes, lightning flashes can be very destructive. 在数百万伏特的电压和数万安培的电流作用下，雷电 flashes 可以造成极大的破坏。 Most of the information in this section comes from E. R. Williams' Scientific American article "The Electrification of Thunderstorms" or from Martin Uman's classic book "Lightning". 本节的大部分信息来自E. R. Williams在《科学美国人》上发表的文章《雷暴的电离》或马丁·乌曼的经典著作《雷电》。

Where will lightning strike?

This is certainly a plausible question, and you can answer that it will take the path of least resistance to the Earth. But the classic response is to say "That is like asking where the 800 pound gorilla is going to sit. Anywhere he wants!" That is not to say that there are no physical laws involved, it is just that there are many variables and a degree of chaos in the environment of the charge. In a medium which could be classified as "nonlinear", implying that it doesn't follow simple proportionalities, the path of the lightning strike is not predictable in practice. As an example of this kind of variability, electric discharges can be produced with a Tesla coil. The path of the discharge changes drastically with time, even though the voltage and the nature of the surrounding air are reasonably constant.

Dipole Models for Cloud Charging

Tripolar model, cloud charging

In addition to the positive region at the top of a thundercloud and the main negative N-region near the bottom, a smaller positive region called the p-region has been observed at the bottom of the cloud. This positive region is thought to be important in the triggering of the most common cloud-to-ground discharges. According to Williams, the N-region is a thin, pancake shaped layer of thickness less than a kilometer but which may extend several kilometers horizontally. It is typically at a height of about 6 km, and lightning discharges are typically some 3 km long in cloud-to-ground discharges.