Discussion
Which asymmetry produces the foehn warming?
Answer: A
Air rising and condensing cools at about 5 kelvin per kilometre, but once the moisture has fallen out as precipitation the descending air warms at 9.8, so it arrives warmer and much drier. The temperature difference across a 3 kilometre barrier can exceed 10 kelvin. The precipitation on the windward side is essential to the mechanism.
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