Discussion
Which cloud results from convection confined beneath an inversion?
Answer: D
An inversion caps the ascent, so the cloud spreads laterally at that level and develops the flattened top characteristic of fair weather cumulus beneath a subsidence inversion. Deep convection requires the cap to be absent or broken. Altocumulus castellanus indicates elevated instability and is a genuine sign of potential for later development, which makes it an instructive distractor. Working one numerical case through both cases side by side fixes the distinction better than any rule of thumb.
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