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Turbulent fluxes of momentum, heat, and moisture across the air-sea interface control the transfer of energy and mass between the atmosphere and ocean and therefore play a vital role in weather and climate (Komen et al., 1996). Turbulent fluxes have been explored extensively using measurements, theoretical and numerical models, and laboratory experiments. In past decades, the impacts of surface waves (including swells) on air-sea interactions have attracted the attention of the research community. Studies show that waves can significantly affect these turbulent fluxes (
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