摘要: Under high wind speed conditions breaking waves disrupt the air-sea interface producing a two-phase zone—air bubbles in water and sea spray air. This mixed-phase environment changes regime of interaction. In this chapter, after reviewing dynamics air-bubbles droplets detail, reader is exposed to idea that under strong winds Kelvin-Helmholtz instability likely mechanism for intense production spume formation transition layer. The resulting eliminates short wind-waves, including some responsible substantial part surface stress. Amazingly, concept provides an explanation rapid intensification storms major tropical cyclones observed bi-modal distribution cyclone maximum intensity. A long overdue implementation micro-physics into operational models expected improve predictions intensity associated wave field.
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