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Print viewElectrical specs of earth lightning

Cloud-to-earth lightning has the greatest damage potential. This type of lightning is divided into positive and negative lightning, depending on the polarity of the cloud charge.

Positive cloud-to-earth lightning is the most critical, due to the duration of the lightning current pulse. With a maximum current of several 10 kA, it may last longer than 2 ms. The electrical charge is typically higher than 50 As.

Negative cloud-to-earth lightning starts with a lightning current pulse whose maximum amplitude amounts also to several 10 kA, but lasts merely 1/10 of the time of a positive one. Its peculiarity lies in the subsequent smaller multiple discharges, which may result in a total duration of the lightning of over one second and a total electrical discharge of over 100 As.



Time domain considerations - Currents

This produces the following basic, schematic lightning current patterns:


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1) Positive or negative lightning current pulse of several 10 kA and less than 2 ms duration  (TS).


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2) Positive or negative lightning current pulse according to 1), with subsequent long-duration current of about 100 A during a period of less than 500 ms (TI).

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3) Sequence of negative lightning currents with a first lightning current pulse according to 1), followed by subsequent lightning currents up to 10 kA. The break
times between the lightning current pulses
are shorter than 100 ms.

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4) Sequence of negative lightning currents according to 3), with integral long-duration current according to 2)
On the basis of these lightning current patterns, CIGRÉ and IEC 61312-1 defined 3 groups of laboratory-simulated lightning currents:

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Group 1 – lightning current of positive or negative polarity, first stroke – wave form 10/350 µs


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Group 2 – lightning current of negative polarity, subsequent stroke – wave form 0.25/100 µs

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Group 3 – lightning current of positive or negative polarity, long-duration stroke – DC 0.5 s

The most important parameters of lightning are the following:
Lightning current amplitude iL – determines the resistive effects mentioned below

Average steepness of the lightning current diL / dt – determines the resistive and magnetic coupling effects mentioned below

Total charge Q = L * dt (unit As or C) – determines the energy release/conversion at the hit point

Specific energy  (action integral)
W/R = L2 * dt (unit MJ/ or kA2s) – determines all heating and electrodynamic effects along the down-conducting path.

Group 3 – lightning current of positive or negative polarity, long-duration stroke – DC 0.5 s

The most important parameters of lightning are the following:
Lightning current amplitude iL – determines the resistive effects mentioned below

Average steepness of the lightning current diL / dt – determines the resistive and magnetic coupling effects mentioned below

Total charge Q = L * dt (unit As or C) – determines the energy release/conversion at the hit point

Specific energy  (action integral)
W/R = L2 * dt (unit MJ/ or kA2s) – determines all heating and electrodynamic effects along the down-conducting path.

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