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arXiv 2011.13366physics.flu-dyn
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林冠流拉格朗日统计量的小尺度和大尺度不稳定性

On small-scale and large-scale intermittency of Lagrangian statistics in canopy flow

Ron Shnapp

摘要:

在冠层流动中,流体与表面安装的障碍物的相互作用导致强烈的湍流,在中性稳定的大气表面层中主导着分散和混合。这项工作的重点是在拉格朗日速度统计的冠层流,这是观察到两种不同的形式。第一,小规模的不稳定性,表示由非高斯和不自相似的统计的速度增量。分析表明,与以前的结果比较一致,从均匀各向同性湍流(HIT)使用多重分形模型,扩展的自相似性,和加速度自相关。这些观测结果表明,冠层流中的小尺度拉格朗日不稳定性的图像与HIT中的图像相似,因此,它们将通用拉格朗日不稳定性的思想扩展到某些非均匀和各向异性流。其次,它是观察到的能量增量的RMS沿拉格朗日轨迹依赖于轨迹的时间平均湍流速度的方向。随后的分析表明,流被冠层阻力衰减,而结构函数的标度不变。这一观测结果意味着拉格朗日统计量中存在大尺度不稳定性。因此,这项工作提出了第一个经验证据的间歇拉格朗日速度统计在冠层流存在于两个不同的意义上,发生由于不同的机制。

英文摘要:

The interaction of fluids with surface-mounted obstacles in canopy flows leads to strong turbulence that dominates dispersion and mixing in the neutrally stable atmospheric surface layer. This work focuses on intermittency in the Lagrangian velocity statistics in a canopy flow, which is observed in two distinct forms. The first, small scale intermittency, is expressed by non-Gaussian and not self-similar statistics of the velocity increments. The analysis shows an agreement in comparison with previous results from homogeneous isotropic turbulence (HIT) using the multifractal model, extended self-similarity, and acceleration autocorrelations. These observations suggest that the picture of small-scale Lagrangian intermittency in canopy flows is similar to that in HIT, and therefore, they extend the idea of universal Lagrangian intermittency to certain inhomogeneous and anisotropic flows. Second, it is observed that the RMS of energy increments along Lagrangian trajectories depend on the direction of the trajectories' time-averaged turbulent velocity. Subsequent analysis suggests that the flow is attenuated by the canopy drag while leaving the structure function's scaling unchanged. This observation implies the existence of large-scale intermittency in Lagrangian statistics. Thus, this work presents a first empirical evidence of intermittent Lagrangian velocity statistics in a canopy flow that exists in two distinct senses and occurs due to different mechanisms.

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