Scientific and technical challenges in designing the air-sea interface module in tropical cyclone conditions will be discussed, with a particular focus on the effects of breaking waves and sea sprays. Breaking waves may significantly modify the air-sea momentum flux. They cause airflow separation behind breaking wave crests and become responsible for most of the air-sea momentum flux in very young developing seas. Wave breaking limits the steepness of smaller waves and their contribution to the form drag. Sea sprays, generated in great amount by surface breaking waves in high winds, may reduce the near surface atmospheric boundary layer turbulence, leading to reduced friction at the air-sea interface. However, it is difficult to accurately quantify this effect because of the large uncertainty in the spray generation function.
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