2013 International Symposium on Lightning Protection (XII SIPDA) 2013
DOI: 10.1109/sipda.2013.6729246
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CIGRE technical brochure on lightning parameters for engineering applications

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Cited by 47 publications
(19 citation statements)
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“…Another study from 2013 challenged some of the traditional parameters used. For example, they estimated that more than 80% of negative cloud-toground lightning flashes are composed of two or more strokes with the average being 3 to 5 strokes [17]. They also found that even though the first stroke has 2 to 3 times the peak current on average, about 1/3 of flashes have at least one subsequent stroke that exceeds the peak current of the first stroke.…”
Section: Lightning Parametersmentioning
confidence: 99%
“…Another study from 2013 challenged some of the traditional parameters used. For example, they estimated that more than 80% of negative cloud-toground lightning flashes are composed of two or more strokes with the average being 3 to 5 strokes [17]. They also found that even though the first stroke has 2 to 3 times the peak current on average, about 1/3 of flashes have at least one subsequent stroke that exceeds the peak current of the first stroke.…”
Section: Lightning Parametersmentioning
confidence: 99%
“…Típicamente el primer pico de la corriente (A) es de un factor de 2 a 3 veces más grande que las corrientes pico de las descargas subsecuentes. Sin embargo, cerca de un tercio de las descargas de nube a tierra, llevan al menos una descarga subsecuente con una intensidad de campo eléctrico mayor que la del primer pico [12]. Figura 1.…”
Section: Introduccionunclassified
“…Existe uma variedade de funções que representam as formas de onda de corrente dos surtos presentes na literatura, como pode ser visto em Rakov et al (2013), entre elas as principais são a dupla rampa, a dupla exponencial e a função de Heidler (Figura 25). As funções dupla rampa e dupla exponencial são amplamente utilizadas para análises de descargas.…”
Section: Surto Atmosféricounclassified
“…Geralmente, um surto atmosférico é o conjunto de três descargas que ocorrem, tipicamente, em intervalos que variam de 20 à 50 milissegundos. Como o intervalo de tempo entre as descargas subsequentes é suficientemente longo, o efeito transitório é dissipado antes que outras ocorram, e suas amplitudes podem ser consideradas independentemente para uma análise (RAKOV et al, 2013;SALIMI, 2017).…”
Section: Surto Atmosféricounclassified
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