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Comparison of conventional Lagrangian stochastic footprint models against LES driven footprint estimates

机译:传统的拉格朗日随机足迹模型与LES驱动的足迹估计的比较

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In this study we introduce a comparison method for footprint model resultsby evaluating the performance of conventional Lagrangian stochastic (LS) footprintmodels that use parameterised flow field characteristics with results of a Lagrangiantrajectory model embedded in a large eddy simulation (LES) framework. The two conventional models followthe particles backward and forward in time while the trajectories in LES onlyevolve forward in time. We assess their performance in two unstably stratified boundary layersat observation levels covering the whole depth of the atmospheric boundary layer.We present a concept for footprint model comparison that can be applied for 2-Dfootprints and demonstrate that comparison of only cross wind integratedfootprints is not sufficient for purposes facilitating two dimensional footprint information.Because the flow field description among the three models is most realisticin LES we use those results as the reference in the comparison.We found that the agreement of the two conventional models against the LESis generally better for intermediate measurement heights and for the moreunstable case, whereas the two conventional flux footprint models agree bestunder less unstable conditions. The model comparison in 2-D was found quitesensitive to the grid resolution.
机译:在这项研究中,我们通过评估使用参数化流场特征的传统拉格朗日随机(LS)足迹模型的性能以及嵌入大型涡流仿真(LES)框架中的拉格朗日轨迹模型的结果,介绍了一种足迹模型结果的比较方法。两种常规模型都跟随粒子在时间上向前和向后移动,而LES中的轨迹仅在时间上向前移动。我们在覆盖大气边界层整个深度的两个观测层上评估了它们在不稳定的分层边界层中的性能。我们提出了一种足迹模型比较的概念,该概念可以应用于2英尺足迹,并且证明仅交叉风综合足迹的比较是不够的为了方便二维足迹信息,因为在LES中这三个模型之间的流场描述是最现实的,所以在比较中我们将这些结果作为参考。我们发现,两个常规模型相对于LES的一致性通常更好地用于中间测量高度和更不稳定的情况,而两个常规的磁通量足迹模型在不稳定程度较小的情况下最佳吻合。发现二维中的模型比较对网格分辨率非常敏感。

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