Discussion
Which stability structure does the land breeze possess?
Answer: D
The offshore flow is itself a shallow cold layer, but as it crosses the warmer water it is heated from below and destabilises, which is why convection can develop offshore at night. Both descriptions are therefore partly right depending on how far offshore one looks. The initial structure close to the coast is the stable one, which is what the question asks about. The quantity that varies and the quantity that does not are worth naming before any substitution is attempted.
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