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A COMPARISON OF WIND-TUNNEL EXPERIMENTS AND NUMERICAL SIMULATIONS OF NEUTRAL AND STRATIFIED FLOW OVER A HILL

机译:山丘中空和分层流动的风洞实验与数值模拟比较

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摘要

A comparison is made of numerical and experimental results for flow over two-dimensional hills in both neutral and stably stratified flow. The numerical simulations are carried out using a range of one-and-a-half order and second-order closure schemes. The performance of the various turbulence schemes in predicting both the mean and turbulent quantities over the hill is assessed by comparing the results with new wind-tunnel measurements. The wind-tunnel experiments include both neutral and stably stratified flow over two different hills with different slopes, one of which is steep enough to induce flow separation. The dataset includes measurements of the mean and turbulent parts of the flow using laser Doppler anemometry. Pressure measurements are also made across the surface of the hill. These features make the dataset an excellent test of the model performance. In general second-order turbulence schemes provide the best agreement with the experimental data, however, they can be numerically unstable for steep hills. Some modifications can be made to the standard one-and-a-half order closure scheme, which results in improved performance at a fraction of the computation cost of the second-order schemes.
机译:比较了中性和稳定分层流中二维山丘上的流动的数值和实验结果。数值模拟是使用一系列的半阶和二阶闭包方案进行的。通过将结果与新的风洞测量结果进行比较,可以评估各种湍流方案在预测山上的平均和湍流量方面的性能。风洞实验包括在两个具有不同坡度的不同山丘上的中性流和稳定分层流,其中一个坡度足以引起流分离。该数据集包括使用激光多普勒风速计测量的平均和湍流部分的测量值。压力测量也在整个山体表面进行。这些功能使数据集成为模型性能的绝佳测试。通常,二阶湍流方案可以提供与实验数据的最佳一致性,但是,对于陡峭的山坡,它们在数值上可能不稳定。可以对标准的一个半半闭包方案进行一些修改,从而以较低的二阶方案的计算成本提高性能。

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