doi:  10.3878/j.issn.1006-9895.2003.19239
重庆城市热岛环流结构和湍流特征的数值模拟

A Numerical Simulation of Urban Breeze Circulation Structure and its Turbulence Characteristics in Chongqing
摘要点击 56  全文点击 18  投稿时间:2019-10-26  修订日期:2020-03-16
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基金:  国家重点研发计划重点专项项目2018YFC1506902;重庆市社会事业与民生保障科技创新专项CSTC2015SHMSZX00010;中国气象局省级气象科研所科技创新发展经费项目SSCX201917
中文关键词:  复杂地形  城市热岛环流 山谷风  江陆风 湍流动能  湍流通量
英文关键词:  Complex terrain  Urban heat island circulation  Mountain-valley breeze  River-land breeze  Turbulent kinetic energy  Turbulent flux
        
作者中文名作者英文名单位
朱 丽ZHU Li南京信息工程大学气象灾害教育部重点实验室
苗峻峰Miaojunfeng南京信息工程大学气象灾害教育部重点实验室
高阳华Gaoyanghua重庆市气象科学研究所
引用:朱 丽,苗峻峰,高阳华.2020.重庆城市热岛环流结构和湍流特征的数值模拟[J].大气科学
Citation:ZHU Li,Miaojunfeng,Gaoyanghua.2020.A Numerical Simulation of Urban Breeze Circulation Structure and its Turbulence Characteristics in Chongqing[J].Chinese Journal of Atmospheric Sciences (in Chinese)
中文摘要:
      本文利用中尺度模式WRF V3.9对2016年8月17日~18日重庆一次城市热岛环流个例进行了数值模拟,探讨了山地城市热岛环流的三维结构和演变特征,分析了热岛环流期间湍流动能和各项湍流通量的特征。结果表明:15:00乡村风开始出现,随着热岛强度增强乡村风增强,18:00热岛环流结构最显著,次日02:00热岛环流结构被破坏,仅低层存在微弱的乡村风。其中,重庆市城市热岛环流最强时,水平尺度约城市尺度的1.5~2倍,垂直厚度约1.3 km,水平风速约2~4 m?s-1,最大上升速度约0.5 m?s-1。受地形、河流以及背景风的影响,环流呈现非对称的结构,且强度较弱。分析湍流特征发现,城市区域的湍流动能明显大于非城市区域,湍流动能的非均匀分布造成城市区域湍流对热量和水汽的输送较非城市区域强。此外,城市热岛环流对湍流水汽通量的影响明显;湍流动量通量补充边界层中因热岛环流发展而造成的动量耗散。
Abstract:
      To investigate the structure and evolution characteristics of urban breeze circulation in the mountain city, WRF V3.9 is used to simulate a typical urban breeze circulation case from August 17 to 18, 2016 in Chongqing. In addition, the characteristics of turbulent kinetic energy and turbulent fluxes during this period are also analyzed. The results show that the rural wind begins to appear at 15:00 and increases as the heat island strengthen. The circulation reaches its maximum at 18:00, and is destroyed at 02:00 in the next day. At 18:00, the horizontal scale of the circulation is about 1.5~2 times that of the urban scale, and the vertical scale is about 1.3 km, the horizontal wind speed is about 2~4 m?s-1, the maximum rising speed is about 0.5 m?s-1. Under the influence of topography, rivers and background wind, the circulation is asymmetrical in structure and weak in intensity. Besides, it is found that the turbulent kinetic energy in the urban area is obviously larger than that in the nonurban area, which results in the stronger transport of heat and water vapor by turbulence in the urban area. When it comes to the relationship between turbulent fluxes and urban breeze circulation, it shows that turbulent water vapor flux is affected by urban breeze circulation obviously, turbulent supply momentum for the dissipation caused by urban breeze circulation.
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