Discussion
Which process most often breaks a capping inversion?
Answer: A
Heating warms the mixed layer from below while synoptic scale ascent cools and lifts the inversion from above, and the two together erode it. Convergence along a boundary can also provide the localised lift required. Subsidence strengthens the cap, and lowering the condensation level makes the parcel path warmer rather than helping it penetrate the cap. A limit that survives making every external component ideal is an intrinsic one, and worth knowing for that reason.
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