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Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes

机译:能量和流量预算(EFB)紊流闭合模型,用于稳定地分层流动。第一部分:稳态,同质状态

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We propose a new turbulence closure model based on the budget equations for the key second moments: turbulent kinetic and potential energies: TKE and TPE (comprising the turbulent total energy: TTE = TKE + TPE) and vertical turbulent fluxes of momentum and buoyancy (proportional to potential temperature). Besides the concept of TTE, we take into account the non-gradient correction to the traditional buoyancy flux formulation. The proposed model permits the existence of turbulence at any gradient Richardson number, Ri. Instead of the critical value of Richardson number separating—as is usually assumed—the turbulent and the laminar regimes, the suggested model reveals a transitional interval, $0.1 < {rm Ri} < 1$ , which separates two regimes of essentially different nature but both turbulent: strong turbulence at ${rm Ri} ll 1$ ; and weak turbulence, capable of transporting momentum but much less efficient in transporting heat, at ${rm Ri} > 1$ . Predictions from this model are consistent with available data from atmospheric and laboratory experiments, direct numerical simulation and large-eddy simulation.
机译:我们基于关键的第二时刻的预算方程,提出了一个新的湍流闭合模型:湍动能和势能:TKE和TPE(包含湍流总能量:TTE = TKE + TPE)以及动量和浮力的垂直湍流(比例)到潜在温度)。除了TTE的概念外,我们还考虑了对传统浮力通量公式的非梯度校正。所提出的模型允许在任何梯度的理查森数Ri处都存在湍流。建议的模型显示了一个过渡区间$ 0.1 <{rm Ri} <1 $,而不是通常认为的理查森数分离的临界值(湍流和层流状态),该间隔将本质上不同的两个状态分隔开来湍流:在$ {rm Ri} ll 1 $时有强烈湍流; $ {rm Ri}> 1 $时,湍流较弱,能够传递动量,但传递热量的效率低得多。该模型的预测与来自大气和实验室实验,直接数值模拟和大涡模拟的可用数据一致。

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