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Frente pseudocálido

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En meteorología, un frente pseudocálido es un límite entre la región de flujo entrante y la corriente descendente del flanco delantero de una supercélula. Puede estar estacionario o moverse en dirección noreste.[1]​ Si fuera estacionario, técnicamente sería un frente pseudoestacionario.

Véase también

Referencias

  1. ↑ Branick, Michael. «A Comprehensive Glossary of Weather». Consultado el 28 de mayo de 2007. 

Enlaces externos

Esta página se editó por última vez el 1 sep 2023 a las 15:57.
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