Lifecycle of the Thunderstorm

Lifecycle of the Thunderstorm

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Description

Cumulonimbus (Cb) (Cb) clouds, in which Thunderstorms are found, form when three conditions are met:

  • There must be a deep layer of unstable air.
  • The air must be warm and moist.
  • A trigger mechanism must cause the warm moist air to rise:
    • Heating of the layer of air close to the surface.
    • Rising ground forcing the air upwards (orographic uplift).
    • A front forcing the air upwards.

A Cumulonimbus Cloud develops in three distinct phases:

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