HIGHLIGHTS
SUMMARY
If mountainous terrain (which certainly is complex) should alter the exchange efficiency, this would impact not only the understanding of mountain weather and climate itself, but also the state of the atmosphere. In this contribution the authors argue that the authors cannot a priori assume that the exchange over mountainous terrain is governed by the same processes as that over flat and homogeneous terrain. Adapted from Lehner and Rotach. and climate modeling, and understanding of transport and exchange processes over mountainous terrain. This means that when numerical models use surface exchange parameterizations based on . . .
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