Estimation and characterisation of the wave-induced turbulent kinetic energy and turbulent dissipation from ADCP data

Clément Calvino, A. Bennis, L. Furgerot, Bailly du Bois Pascal, Poizot Emmanuel
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Abstract

Turbulence in the water flow causes small-scale variations in the mechanical stress acting on submerged tidal turbines. As such it increases their fatigue loading and impacts greatly their lifetime. It is therefore essential for engineers to have an accurate knowledge and characterisation of turbulence at a given site as they design the structures to be deployed. The strength of the tidal currents is the main parameter influencing the intensity of turbulence through their friction with the sea bed. However, most potential tidal energy sites are located in a coastal environment with shallow enough water depths so that the direct impact of waves on turbulence can not be overlooked. Steepness-induced wave breaking is indeed observed to increase the turbulent mixing for such applications. In this context, we propose to estimate the contribution of surface processes to the total turbulence in Alderney Race, France, the most energetic tidal site in western Europe. The turbulent kinetic energy (TKE) specifically induced by waves and wind is characterised using measurements from a 5-beams ADCP deployed between 27/02/2018 and 06/07/2018.Analytical profiles are fitted to the data, the only fitting parameter of the model is an evaluation of the turbulence penetration depth, it determines how deep surface processes impact the water column. Its dependence towards mean wave and current parameters is studied. The results do not allow to conclude on the nature of turbulence observed in the mid water column.
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从ADCP数据估计和表征波浪诱导湍流动能和湍流耗散
水流中的湍流引起作用在水下潮汐涡轮机上的机械应力的小范围变化。因此,它增加了它们的疲劳载荷,极大地影响了它们的寿命。因此,工程师在设计要部署的结构时,对给定地点的湍流有准确的了解和特征是至关重要的。潮汐流的强度是影响湍流强度的主要参数,潮汐流通过与海床的摩擦作用影响湍流强度。然而,大多数潜在的潮汐能站点位于水深足够浅的沿海环境中,因此波浪对湍流的直接影响不容忽视。在这类应用中,陡度引起的破波确实增加了湍流混合。在这种情况下,我们建议估计地表过程对西欧最具活力的潮汐地点法国奥尔德尼海的总湍流的贡献。利用在2018年2月27日至2018年7月6日部署的5束ADCP测量数据,对波浪和风引起的湍流动能(TKE)进行了表征。分析剖面拟合数据,模型的唯一拟合参数是湍流渗透深度的评价,它决定了地表过程对水柱的影响程度。研究了其对平均波和电流参数的依赖关系。这些结果不能对在中部水柱观测到的湍流性质作出结论。
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