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Linking a Lagrangian Particle Dispersion Model with Three-Dimensional Eulerian Wind Field Models

机译:将拉格朗日粒子色散模型与三维欧拉风场模型链接

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摘要

A slightly simplified form of Thomson's Lagrangian stochastic model (LSM) is presented for dispersion applications in three-dimensional (3D) flow fields. It is found that the Lagrangian velocity of a particle in 3D inhomogeneous Gaussian turbulence can be decomposed into the local Eulerian mean velocity UEi at the particle position and a velocity perturbation u_i. The Eulerian mean wind can be predicted by 3D wind field models, whereas the u_i is obtained from Thomson's model and depends on the turbulence field. The U_(Ei), u_i decomposition was used earlier in a two-dimensional particle model for a canopy (by Flesch and Wilson) and in models with 3D mean winds but with u_i based on LSM forms differing from that of Thomson. This note shows that theU_(Ei), u- decomposition is consistent with Thomson's LSM for general 3D flow fields and is a simpler solution that should lead to improved computational efficiency for dispersion applications.
机译:提出了汤姆森拉格朗日随机模型(LSM)的略微简化形式,以用于三维(3D)流场中的分散应用。发现在3D非均匀高斯湍流中,粒子的拉格朗日速度可以分解为粒子位置的局部欧拉平均速度UEi和速度扰动u_i。欧拉平均风可以通过3D风场模型预测,而u_i是从汤姆森模型获得的,并且取决于湍流场。 U_(Ei),u_i分解较早用于机盖的二维粒子模型(由Flesch和Wilson编写)以及3D平均风模型,但u_i基于不同于Thomson的LSM形式。该说明表明,U_(Ei),u-分解与Thomson的LSM在常规3D流场中的一致性,并且是一种更简单的解决方案,应该会提高分散应用的计算效率。

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