Abstract
An inertia-gravity wave which propagates upwind and upward in the thermocline has a reflection coefficient r which is greater than unity ("overreflection") as a result of the wave current interaction in the mixed layer which overlies the thermocline….
Recommended Citation
Stern, Melvin E.. 1977. "Interaction of inertia-gravity waves with the wind." Journal of Marine Research 35, (3). https://elischolar.library.yale.edu/journal_of_marine_research/1402
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