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Coherent Turbulent Structures Across a Vegetation Discontinuity

机译:植被间断的相干湍流结构

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The study of turbulent flow across a vegetation discontinuity is of significant interest as such landscape features are common, and as there is no available theory to describe this regime adequately. We have simulated the three-dimensional dynamics of the airflow across a discontinuity between a forest (with a leaf area index of 4) and a clearing surface using large-eddy simulation. The properties of the bulk flow, as well as the large-scale coherent turbulent structures across the forest-to-clearing transition and the clearing-to-forest transition, are systematically explored. The vertical transport of the bulk flow upstream of the leading edge gives rise to the enhanced gust zone around the canopy top, while the transport downstream of the trailing edge leads to the formation of a recirculation zone above the clearing surface. The large-scale coherent structures across the two transitions exhibit both similarities with and differences from those upstream of the corresponding transition. For example, the ejection motion is dominant over the sweep motion in most of the region 1 < z/h < 2 (h is the canopy height) immediately downstream of the trailing edge, much as in the forested area upstream. Also, the streamwise vortex pair, which has previously been observed within the canopy sublayer and the atmospheric boundary layer, is consistently found across both transitions. However, the inflection observed both in the mean streamwise velocity, as well as in the vertical profiles of the coherent structures in the forested area, disappears gradually across the forest-to-clearing transition. The coherence of the turbulence, quantified by the percentage of the total turbulence kinetic energy that the coherent structures capture from the flow, decreases sharply immediately downstream of the trailing edge of the forest and increases downstream of the leading edge of the forest. The effects of the ratio of the forest/clearing lengths under a given streamwise periodicity on flow statistics and coherent turbulent structures are presented as well.
机译:跨植被不连续性的湍流研究非常重要,因为这种景观特征很普遍,并且由于没有可用的理论来充分描述这种情况。我们使用大涡模拟来模拟穿过森林(叶面积指数为4)和清洁表面之间的不连续性的气流的三维动力学。系统地研究了从森林到砍伐过渡和从砍伐到森林过渡的大流量特性以及大规模连贯的湍流结构。在前缘上游的大流量的垂直输送引起围绕冠层顶部的增强的阵风区域,而在后缘下游的输送导致在清洁表面上方形成再循环区域。跨越两个过渡的大规模相干结构与相应过渡的上游结构既相似又不同。例如,在后缘下游的大部分区域z / h <2(h是树冠高度)中,顶出运动在横扫运动中占主导地位,与上游的林区一样。同样,先前在冠层子层和大气边界层中观察到的沿流方向的涡流对在两个过渡过程中始终存在。然而,在森林中的平均流向速度以及在林区连贯结构的垂直剖面中观察到的拐点,在从森林到砍伐的过渡过程中逐渐消失。湍流的相干性(通过相干结构从流中捕获的总湍流动能的百分比来量化)立即在森林后缘的下游急剧减小,并在森林前缘的下游增大。还给出了在给定的水流周期性下森林/砍伐长度之比对流量统计和相干湍流结构的影响。

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