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Representation of the Reynolds stress tensor through quadrant analysis for a near-neutral atmospheric surface layer flow
Environmental Fluid Mechanics ( IF 1.7 ) Pub Date : 2019-05-06 , DOI: 10.1007/s10652-019-09689-7
Subharthi Chowdhuri , Pramit Kumar Deb Burman

To disseminate the role of the eddy motions on the anisotropic states of the Reynolds stress tensor (\(\varvec{B}\)), we devise a novel methodology based on the quadrant analysis, where the distributions of the invariants of \(\varvec{B}\) are studied on a \(u^{\prime }\)\(w^{\prime }\) quadrant plane, with \(u^{\prime }\) and \(w^{\prime }\) being the turbulent fluctuations in the streamwise and vertical velocities. We apply this methodology to a near-neutral atmospheric surface layer (ASL) flow, derived from a field experiment dataset having multi-level turbulence measurements. The results show that in a near-neutral ASL flow, the anisotropic states of \(\varvec{B}\) are determined by the distribution of the streamwise and cross-stream velocity variances (\(\sigma _{u}^2\) and \(\sigma _{v}^2\)) on the \(u^{\prime }\)\(w^{\prime }\) quadrant plane. By studying the contour maps of the invariants of \(\varvec{B}\) on the \(u^{\prime }\)\(w^{\prime }\) quadrant plane, we discover three distinct zones with elliptical boundaries in the \(u^{\prime }\)\(w^{\prime }\) plane, across which the anisotropic states of the eddy motions evolve. We find that the eddy motions which occur
  1. 1.Inside the inner elliptical zone display rod-like anisotropy being determined by \(\sigma _{v}^2\),
  2. 2.Within the annular zone between the inner and outer ellipses display pancake-like anisotropy being determined by both \(\sigma _{u}^2\) and \(\sigma _{v}^2\),
  3. 3.Outside the outer elliptical zone display rod-like anisotropy being determined by \(\sigma _{u}^2\).
We also notice that the distinction between these three zones in the \(u^{\prime }\)\(w^{\prime }\) plane is prominent at the lowest measurement level, but becomes progressively indistinguishable as the measurement height increases.


中文翻译:

雷诺应力张量通过象限分析表示为近似中性的大​​气表层流动

为了传播涡动运动对雷诺应力张量各向异性状态(\(\ varvec {B} \))的作用,我们基于象限分析设计了一种新颖的方法,其中\(\ varvec {B} \)\(u ^ {\ prime} \)\(w ^ {\ prime} \)象限平面上研究,其中\(u ^ {\ prime} \)\(w ^ {\ prime} \)是沿流向和垂直速度的湍流波动。我们将此方法应用于近中性大气表层(ASL)流动,该流动是从具有多级湍流测量值的现场实验数据集中得出的。结果表明,在接近中性的ASL流中,\(\ varvec {B} \)的各向异性状态\(u ^ {\ prime)上的流向和跨流速度方差(\(\ sigma _ {u} ^ 2 \)\(\ sigma _ {v} ^ 2 \)的分布确定} \)\(w ^ {\ prime} \)象限平面。通过研究轮廓的不变量的映射\(\ varvec {B} \)\(U ^ {\黄金} \) - \(W ^ {\黄金} \)象限飞机,我们发现有三个不同的区域\(u ^ {\ prime} \)\(w ^ {\ prime} \)平面中的椭圆边界,涡旋运动的各向异性状态在该边界上演化。我们发现发生的涡流运动
  1. 1.在内部椭圆区内,显示由\(\ sigma _ {v} ^ 2 \)确定的棒状各向异性,
  2. 2.在内部和外部椭圆之间的环形区域内,显示出由\(\ sigma _ {u} ^ 2 \)\(\ sigma _ {v} ^ 2 \)决定的煎饼状各向异性,
  3. 3.在外部椭圆形区域之外,显示由\(\ sigma _ {u} ^ 2 \)确定的棒状各向异性。
我们还注意到,在最低测量级别,\(u ^ {\ prime} \)\(w ^ {\ prime} \)平面中的这三个区域之间的区别很明显,但随着测量高度的逐渐变得无法区分增加。
更新日期:2019-05-06
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