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The Effect of Surface Heating on Hill-Induced Flow Separation

机译:地表加热对丘陵诱导流分离的影响

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A series of two-dimensional mixing length model simulations of boundary-layer flow over idealised ridges of varying steepness are conducted to investigate the effect of surface heating on flow separation. The relatively simple numerical approach used permits characterisation of the influence of heating for a variety of initial conditions and parameter values. For steep terrain, increased surface heating is shown to enhance the strength and extent of hill-induced separation. For more moderate terrain, a critical heating strength is required for a given hill width and background flow speed before separation is initiated. Sensitivity tests show the results to be insensitive to model parameters or the choice of mixing length. The results are accounted for using a scaling analysis in terms of a non-dimensional stability parameter.
机译:进行了一系列二维混合长度模型,模拟了不同陡度的理想脊上边界层的流动,以研究表面加热对流动分离的影响。所使用的相对简单的数值方法可以表征各种初始条件和参数值的加热影响。对于陡峭的地形,增加的地表加热可以增强山坡引起的分离的强度和程度。对于较平缓的地形,在开始分离之前,对于给定的山坡宽度和背景流速,需要一个临界加热强度。敏感性测试表明结果对模型参数或混合长度的选择不敏感。使用缩放分析根据无量纲稳定性参数说明了结果。

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