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Study on Effects of Building Morphology on Urban Boundary Layer Using an Urban Canopy Model

机译:利用城市冠层模型研究建筑形态对城市边界层的影响

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摘要

An urban canopy model is incorporated into the Nanjing University Regional Boundary Layer Model. Temperature simulated by the urban canopy model is in better agreement with the observation, especially in the night time, than that simulated by the traditional slab model. The coupled model is used to study the effects of building morphology on urban boundary layer and meteorological environment by changing urban area, building height, and building density.It is found that when the urban area is expanded, the urban boundary layer heat flux, thermal turbulence, and the turbulent momentum flux and kinetic energy all increase or enhance, causing the surface air temperature to rise up. The stability of urban atmospheric stratification is affected to different extent at different times of the day.When the building height goes up, the aerodynamic roughness height, zero plane displacement height of urban area, and ratio of building height to street width all increase. Therefore, the increase in building height results in the decrease of the surface heat flux, urban surface temperature, mean wind speed, and turbulent kinetic energy in daytime. While at night, as more heat storage is released by higher buildings, thermal turbulence is more active and surface heat flux increases, leading to a higher urban temperature.As the building density increases, the aerodynamic roughness height of urban area decreases, and the effect of urban canopy on radiation strengthens. The increase of building density results in the decrease in urban surface heat flux, momentum flux, and air temperature, the increase in mean wind speed, and the weakening of turbulence in the daytime. While at night, the urban temperature increases due to the release of more heat storage.
机译:城市冠层模型被纳入南京大学区域边界层模型。与传统平板模型所模拟的温度相比,城市冠层模型所模拟的温度与观测值(尤其是在夜间)与观测值更加吻合。通过耦合模型研究了建筑物形态对城市边界层和气象环境的影响,包括改变城市面积,建筑物高度和建筑物密度,发现当城市面积扩大时,城市边界层的热通量,热湍流,湍流动量通量和动能都增加或增强,导致地表空气温度升高。在一天中的不同时间,城市大气分层的稳定性受到不同程度的影响。当建筑物高度升高时,空气动力学粗糙度高度,市区零平面位移高度以及建筑物高度与街道宽度的比率都会增加。因此,建筑物高度的增加导致白天的表面热通量,城市表面温度,平均风速和湍动能降低。在夜间,随着高层建筑释放更多的热量,热湍流更加活跃,地表热通量增加,从而导致更高的城市温度。随着建筑物密度的增加,市区的空气动力学粗糙度高度降低,从而产生了影响城市雨棚的辐射强度增强。建筑物密度的增加导致城市地表热通量,动量通量和空气温度的降低,平均风速的增加以及白天湍流的减弱。在夜间,由于释放更多的热量,城市温度升高。

著录项

  • 来源
    《气象学报(英文版)》 |2009年第3期|338-349|共12页
  • 作者单位

    Department of Atmospheric Sciences, Nanjing University, Nanjing 210093;

    National Climate Center, China Meteorological Administration, Beijing 100081;

    Department of Atmospheric Sciences, Nanjing University, Nanjing 210093;

    National Climate Center, China Meteorological Administration, Beijing 100081;

    Department of Atmospheric Sciences, Nanjing University, Nanjing 210093;

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  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 大气科学(气象学);
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  • 入库时间 2024-03-26 01:08:14
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