Cálculo de disturbios atmosféricos, a partir del nivel isoceráunico: con datos reales comparativos para Alemania Federal, y curvas características de choque.
Cálculo de disturbios atmosféricos, a partir del nivel isoceráunico
DOI:
https://doi.org/10.15446/ing.investig.n4.28791Keywords:
fenómenos atmosféricos, descargas atmosféricas, nivel isoceráunico, intensidad de las tormentas (es)fenómenos atmosféricos, descargas atmosféricas, nivel isoceráunico, intensidad de las tormentas (en)
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El número de disturbios sobre una línea aérea, debidos a fenómenos atmosféricos, depende en primer lugar del Nivel lsoceraunico del área atacada. Esto significa, cuantos días tormentosos al año son esperados en un área determinada. Como día tormentoso es tomado aquel durante el cual, como mínimo, un trueno es oído. En las cercanías al Ecuador se dan hasta 200 días tormentosos al año. (Amazonas y África Central) mientras que en las proximidades a los polos es prácticamente cero.
References
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Blitzschutz 7. Aufl. Hrsg. von Ausschuss für Blitzableiterbau. Berlin 1963.
Young, F. S. Clayton, J. M. Shielding of Transmission Lines. IEEE Trans. Paper 63-640 (1963) S. 132-154.
Rebske, W.: Beitrag zur Bestimmung der Häufigkeit von Blitzeinschlagen in die Leiterseile von H. S. leitungen. Elektrot. Z (1965) S. 193-197.
Reisner, H. Ergebnisse der neuen VDEW-Storungs.
Müller-Hillebrand, D: Zur Physic der Bletzentladung. LElektrot. Z. (1961) S. 232-249.
Otto Völker. Gewittergefährdung und Überspannungsschutz von Mittelspannungsanlagen. Siemens Zeits. 1968 S. 176-182.
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Copyright (c) 1982 Horacio Torres Sánchez

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