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(一)概述海气相互作用讨论通过海气分界面的动量、能量和物质的交换,以及这些交换对大气和海水的运动的关系。来自太阳辐射的能量全年平均约有80％可透过大气层到达地球表面,其中60％以上被海洋吸收。这些能量又通过海气相互作用从下面加热大气,从而使大气产生运动,随着海水也被驱使运动,最终由大气把大部分热能载运至两极的大气层顶再辐射回天空,以维持海气系
(I) Overview The air-sea interaction discusses the exchange of momentum, energy and matter through the interface of the sea-air interface and the relationship of these exchanges to the movement of the atmosphere and seawater. On average, about 80% of the energy from solar radiation reaches the Earth’s surface through the atmosphere, of which over 60% is absorbed by the ocean. These energies, in turn, heat the atmosphere from below through the interaction of the sea and air, causing movement of the atmosphere. As the sea is also driven to move, most of the heat is eventually carried by the atmosphere to the bipolar upper atmosphere layer and radiated back to the sky to maintain the marine atmosphere