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The first stage is the cumulus cloud stage in which the fluffy cumulus cloud in an unstable (warm and moist near surface and very cold aloft) builds into a towing cumulus. All we have is an updraft! In the next stage, the mature stage rain begins to fall dragging down cool air and evaporating into the downdraft and cooling it. Then we have an updraft and a downdraft together. When the mature thunderstorm reaches way up in the atmospehere to the tropopause (boundary between the layer of the atmospehere where sensible weather occurs and the stratosphere) an anvil shape becomes evident. The final stage is the dissipating stage. The rain and rain cooled air become so dominant that the updraft dies and all that is left is the downdraft. The thunderstorm dies without an updraft.

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Q: What is the sequence the stages of the formation of a thunderstorm?
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