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Which outcome results at high altitudes when persistent surface winds feed moisture inland?

A)Orogenic precipitation increases stream volume
B)Glacial ablation decreases downstream discharge
C)Thermohaline circulation reverses current flows
D)Sublimation rates rapidly elevate channel gradient

💡 Explanation

Orogenic precipitation sharply increases stream volume because moist air rises and cools over mountains, yielding precipitation through adiabatic cooling; therefore runoff occurs there, rather than solely from lowland condensation driven by other processes.

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