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denominan cumulonimbus secas y se forman en condiciones atmosféricas específicas, como en regiones volcánicas o durante erupciones de polvo. En su interior, las partículas de hielo, cristales y gotitas superenfriadas se mueven constantemente debido a corrientes ascendentes y descendentes. Este movimiento provoca la separación de cargas eléctricas: las cargas positivas se concentran en la parte superior de la nube y las negativas en la parte inferior. Cuando la diferencia de potencial eléctrico e
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