wind mixing 中文意思是什麼

wind mixing 解釋
風混合
  • wind : n 1 風;大風,暴風;氣流;【機械工程】壓縮空氣。2 【航海】上風;風向;〈古語〉〈pl 〉方向。3 氣息...
  • mixing : n. 混合;【電影】錄音;【無線電】混頻。
  1. 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 wind stirring is in the opposite direction

    盡管潮汐混合和風的攪動作用均能削弱河流沖淡水浮力引起的垂直層化現象,但是其控制機制有所不同:潮汐混合是通過湍流動能自下向上的耗散來完成的,風攪動的方向恰好相反。
  2. Internal waves are a kind of bridge relating the diapycnal mechanical mixing to external sources of mechanical energy : first, internal waves are driven by wind stress and barotropic tide so that large amount of mechanical energy are transported to abyssal ocean with propagation of internal waves ; second, the mechanical energy can directly be cascaded to mixing through instability and breaking of internal waves

    內波是外界提供的機械能與混合之間聯系的橋梁之一,一方面風和潮汐通過激發內波,將能量向深海和大洋內區傳遞,另一方面,內波的不穩定和破碎直接將機械能串級到小尺度湍流混合中去。開展傾斜地形上內波的傳播以及內潮的產生等方面的研究對海洋混合過程的參數化以及混合對大洋環流的影響等方面的研究具有重要的科學意義。
  3. 07gw in the summer. so the tidal energy dominates the mixing in summer in the study region, and it also at least as important as the wind stress in the winter

    可以認為在渤黃東海中潮能所起的混合作用在夏季要遠遠的超過風所起的作用,而在冬季最保守也與風具有相同的量級。
  4. The ocean circulation is controlled by diapycnal mixing which consists of mechanical mixing and convective mixing. the intensity of mechanical mixing depends on the amount of mechanical energy offered by external processes, among which wind stress and tidal generation force are major sources

    海洋中的湍混合包括機械混合和對流混合,混合的強弱是控制大洋環流的重要因素,其中機械混合的強弱取決于外界機械能的供給,風和潮汐是重要的機械能之源。
  5. The understanding of the effects of atmospheric forcings, including mainly the surface wind stress, net heat flux and buoyant flux, on the dynamical and thermal structure of the ocean surface mixed layer necessitates a proper knowledge of the mechanisms and influences of the different turbulent mixing processes involved in the upper ocean

    海洋上混合層的動力學和熱力學結構特徵主要受到海表風應力、凈熱通量和浮力通量的影響,而混合層的形成與維持依賴于混合層內的湍流生成和湍流垂向混合。
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