海气界面在高风速的激励下,一般在界面上下形成二相混合层。在界面上方是主体空气和沫滴,而在界面下方则为主体海水和气泡。一般认为,风引起沫滴的机制可能有三,即:风切削波峰;波峰上的空气动力学吸引;以及海面气泡破碎。但据现有资料表明,海面产生沫滴的主要机制是气泡的破裂。由于一定速度的气流可以激起海波且使波峰倒 Under the encouragement of high wind speed, the air-sea interface generally forms a two-phase mixed layer above and below the interface. Above the interface is the main air and droplets, while below the interface is the main sea water and bubbles. It is generally believed that there are three possible mechanisms by which the wind causes the droplet, namely: the wind cutting peak; the aerodynamic attraction on the peak; and the breaking of the bubble on the surface of the sea. However, according to the available information, the main mechanism of foam droplet formation on the sea surface is the rupture of bubbles. As a certain speed of the air flow can stir up the sea wave and the peak down