能量变化的实质是，风场的时变性引起了波流相互作用。
The cause of the packet energy variation is wave-flow interaction produced by temporal variation of the wind.
本文研究了波流相互作用情形下波浪对水平流速沿垂向分布的影响。
The effect of wave on vertical distribution of horizontal flow velocity under the interaction of current flow and wave is studied.
沿观测断面方向，水平能通量净收入、底部生成能通量、波流相互作用、湍动能生成率四项基本保持平衡。
Along the observation section, the net horizontal baroclinic energy flux, the bottom generated energy flux and the wave-current interaction are balanced by the turbulence production rate.
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