Both tidal mixing and wind stirring can weaken the vertical stratification induced by freshwater buoyancy, but different mechanisms dominate such a process: tidal mixing is accomplished through the upward dissipation of turbulent kinetic energy whereas wi
Both tidal mixing and wind stirring can weaken the vertical stratification induced by freshwater buoyancy, but different mechanisms dominate such a process: tidal mixing is accomplished through the upward dissipation of turbulent kinetic energy whereas wi
尽管潮汐混合和风的搅动作用均能削弱河流冲淡水浮力引起的垂直层化现象，但是其控制机制有所不同：潮汐混合是通过湍流动能自下向上的耗散来完成的，风搅动的方向恰好相反。