Lightning Return Stroke at Pamela Beeler blog

Lightning Return Stroke. In this chapter, a general picture of downward negative lightning discharges that take place between cloud and ground are described. Learn how the return stroke is the visible flash of lightning, caused by the rapid discharge of electricity from a step leader to a streamer. An electric current wave, called a return stroke, then shoots up the channel, producing a brilliant pulse. Lightning return stroke speed is an important parameter in lightning protection studies. It only takes the current about 1 microsecond to reach its peak. See diagrams and animations of the. Some researchers (e.g., lundholm, 1957 [4]; Typically, a negative flash of lightning will be comprised of an initial stepped leader/return stroke followed by 2 or 3 subsequent dart leaders/return strokes.

Lightning return stroke scheme Download Scientific Diagram
from www.researchgate.net

It only takes the current about 1 microsecond to reach its peak. In this chapter, a general picture of downward negative lightning discharges that take place between cloud and ground are described. Learn how the return stroke is the visible flash of lightning, caused by the rapid discharge of electricity from a step leader to a streamer. Some researchers (e.g., lundholm, 1957 [4]; See diagrams and animations of the. Typically, a negative flash of lightning will be comprised of an initial stepped leader/return stroke followed by 2 or 3 subsequent dart leaders/return strokes. Lightning return stroke speed is an important parameter in lightning protection studies. An electric current wave, called a return stroke, then shoots up the channel, producing a brilliant pulse.

Lightning return stroke scheme Download Scientific Diagram

Lightning Return Stroke Lightning return stroke speed is an important parameter in lightning protection studies. Typically, a negative flash of lightning will be comprised of an initial stepped leader/return stroke followed by 2 or 3 subsequent dart leaders/return strokes. An electric current wave, called a return stroke, then shoots up the channel, producing a brilliant pulse. It only takes the current about 1 microsecond to reach its peak. Lightning return stroke speed is an important parameter in lightning protection studies. In this chapter, a general picture of downward negative lightning discharges that take place between cloud and ground are described. Learn how the return stroke is the visible flash of lightning, caused by the rapid discharge of electricity from a step leader to a streamer. See diagrams and animations of the. Some researchers (e.g., lundholm, 1957 [4];

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