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Effects of Wall Heating on Flow Characteristics in a Street Canyon

机译:壁加热对街道峡谷流动特性的影响

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We develop a large-eddy simulation (LES) model based on a meteorological numerical model for a real scale street-canyon flow with rough building facets heated by a given temperature. The model is applied to a canyon with the aspect ratio of unity fortwo idealized heating scenarios: (1) the roof and the entire upstream wall are heated, named as ‘assisting cases’, and (2) the roof and the entire downstream wall are heated, named as ‘opposing cases’. These facets were heated up to 15 K above the air temperature. A wall function for temperature is proposed for a rough facet with an assumption that the thermal roughness length, z 0T, is much smaller than the aerodynamic roughness length, z 0. It is demonstrated that the sensible heat flux and canyon-air temperature are significantly influenced by the near-facet process that is parametrized by z 0T as the primary factor; other processes such as in-canyon mixing and roof-level exchange are secondary. This new finding strongly suggests that it is vital to choose an appropriate value of z 0T in a numerical simulation of street-canyon flows with the facet-air exchange processes of heat or any scalar. The finding also raises an awareness of the demand for carefully designed laboratory or field experiments of quantifying z 0T values for various urban surfaces. For the opposing cases, an unsteady penetrating narrow updraft zone appears occasionally along the heated wall and this feature is consistent field observations. The unique result indicates the superior capability of LES. The results of this study can be used to guide the parametrization of turbulent processes inside the urban canopy layer.
机译:我们基于气象数值模型开发了一个大涡模拟(LES)模型,该模型用于在给定温度下加热粗糙建筑物小平面的真实比例的街道峡谷流动。该模型适用于纵横比为1的峡谷,适用于两种理想的供热方案:(1)屋顶和整个上游壁都被加热,称为``辅助箱'',(2)屋顶和整个下游壁都被加热加热,称为“对立例”。这些小平面被加热到高于空气温度15K。提出了一个粗糙面的温度壁函数,并假设热粗糙度长度z 0T远小于空气动力学粗糙度长度z0。这表明显热通量和峡谷空气温度显着受以z 0T为主要参数的近面加工的影响;其他过程是次要的,例如峡谷内混合和屋顶高度交换。这一新发现强烈表明,在通过热或任何标量的平面空气交换过程进行的街道峡谷流动的数值模拟中,选择合适的z 0T至关重要。这一发现还提高了人们对精心设计的实验室或野外实验的需求的认识,以量化各种城市表面的z 0T值。对于相反的情况,沿着加热壁偶尔会出现不稳定的穿透狭窄的上升气流区,该特征与实地观测一致。独特的结果表明LES具有卓越的功能。这项研究的结果可用于指导城市冠层内部湍流过程的参数化。

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