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How lightning really works? (video)

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A lightning discharge develops in three stages: first, the collisions between ice particles and water droplets together with gravity separate positive and negative charges inside the thunder cloud and buildup a voltage. Then a discharge grows, forming a so-called streamer-leader tree.

Finally, when a conducting path is created between cloud and ground, the cloud discharges through the so-called return stroke; currents then reach tens or hundreds of kA, and the released Ohmic heat brings the channel temperatures up to 28000 K.

Today some of the hottest topics in lightning research are related to the second stage: the inception, growth and branching of a conducting channel in non-ionized air.

Under normal circumstances, air is a quite poor conductor because free electrons rapidly attach to oxygen molecules. However,in a suffciently strong electric field (higher than 3.2 MV/m in air at standard temperature and pressure) a free electron can gain enough energy to liberate a second electron when it impacts ona molecule,and an ionization avalanche sets in.

However, in most electrical discharges, including lightning, the background electric field is almost everywhere one to three orders of magnitude below the breakdown value.

SOURCE: Lightning Above Clouds – Alejandro Luque

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Edvard Csanyi

Edvard - Electrical engineer, programmer and founder of EEP. Highly specialized for design of LV/MV switchgears and LV high power busbar trunking (<6300A) in power substations, commercial buildings and industry fascilities. Professional in AutoCAD programming. Present on