The tide energy, like familiar water energy, is a kind of renewable energy.
潮汐能和常规水能一样,是一种取之不尽、用之不竭的可再生性能源。
The semi-diurnal and diurnal internal tide energy densities are large on the continental shelf and in the thermocline of the deep sea.
较强内潮在陆坡区超临界地形上生成,并沿波射线方向传播,导致半日潮和全日潮的能量密度在陆坡区温跃层上较强。
Since it is sustained by the wind and tide energy input to the oceans, diapycnal mixing coefficient (DMC) will vary along with the change of external energy input.
海洋中的混合过程是由风和潮汐输入的机械能维持的,这些机械能的变化会导致海洋中混合率的变化。
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