城市峡谷内流态的三维特征研究

L.J. Hunter, G.T. Johnson, I.D. Watson
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引用次数: 162

摘要

峡谷几何形状是城市峡谷内观察到的气流特征的重要决定因素。三种主要的流动形式是:“掠流”流动,“尾迹干涉”流动和“孤立粗糙”流动,遵循Oke(1987年,边界层气候,第2版,Methuen,伦敦)的命名法。水流之间的过渡是由峡谷的几何形状决定的,可以用任意长度/高度(L/H)比的阈值高度/宽度(H/W)比来描述。阈值H/W比的确定以前依赖于反复的风洞实验或反复运行的数值模型,并改变峡谷的几何形状,直到观察到的流动状态发生变化。本文对城市峡谷内典型的三维流动进行了数值研究,确定了标志着流型转换的关键参数。在此基础上,通过分析几个模拟流的水平截面,可以建立流型之间的几何阈值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An investigation of three-dimensional characteristics of flow regimes within the urban canyon

Canyon geometry is an important determinant characteristic airflow regimes observed within urban canyons. Three principal flow regimes are: “skimming” flow, “wake interference” flow and “isolated roughness” flow, following the nomenclature of Oke (1987, Boundary Layer Climates, 2nd edn, Methuen, London). The transition between flows is determined by canyon geometry and can be described in terms of threshold height/width (H/W) ratios for an arbitrary length/height (L/H) ratio.

The determination of threshold H/W ratios has previously relied on repeated wind tunnel experiments or repeated runs of a numerical model, with canyon geometry altered until the observed flow regime changes. The present numerical investigation of typical three-dimensional flows within urban canyons identifies the key parameters which mark transition between flow regimes. On this basis it is possible to establish the geometric thresholds between regimes with analysis of a horizontal cross-section of a few simulated flows.

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