首页 | 本学科首页   官方微博 | 高级检索  
     检索      

城市形态参数对边界层气象条件影响的模拟
引用本文:申冲,沈傲,田春艳,魏晓琳,李磊,王明洁,陈训来,樊琦.城市形态参数对边界层气象条件影响的模拟[J].中国环境科学,2019,39(1):72-82.
作者姓名:申冲  沈傲  田春艳  魏晓琳  李磊  王明洁  陈训来  樊琦
作者单位:1. 中山大学大气科学学院/广东省气候变化与自然灾害研究重点实验室, 广东 广州 510275; 2. 深圳市气象局, 广东 深圳 518040
基金项目:国家重点研发计划(2016YFC0203602);深圳市科创委项目(JCYJ20170306150333250);国家自然科学基金资助项目(91544102,41630422);广州市科技计划项目(201604020028);国家重点研发计划大气专项课题(2016YFC0203305,2016YFC0203600);气象行业专项项目(GYHY201406031)
摘    要:利用耦合城市冠层方案的气象模式WRF,选取高密度城市深圳,通过在模式中设置不同建筑物高度和密度的敏感性试验,研究城市形态参数对边界层气象条件的影响.结果表明:建筑物高度和密度增加会使日间城市冠层对热量的截留作用增强,城市储热分别增加约6W/m2和9W/m2;在城市冠层遮蔽效应和截限作用的共同影响下,建筑物高度增加会使日间地表温度降低约0.3℃,而建筑物密度增大则会引起地表温度增加0.6℃以上,2m温度和地表温度的变化有很好的一致性.城市建筑物高度和密度增加均会引起地表粗糙度增加,造成风速分别降低约0.4m/s和0.6m/s,同时在夜间,由于湍流运动增强,使得夜间边界层高度分别增加约30~40m和20~30m.反之,建筑物高度和密度减小使日间储热减小6~7.5W/m2,10m风速增加约0.3m/s和0.4m/s,夜间边界层高度降低约30~50m和10~30m.

关 键 词:城市形态  气象要素  WRF  城市冠层方案  
收稿时间:2018-06-21

Assessment of urban morphological structure parameters effects on meteorological fields in planetary boundary layer
SHEN Chong,SHEN Ao,TIAN Chun-yan,WEI Xiao-lin,LI Lei,WANG Ming-jie,CHEN Xun-lai,FAN Qi.Assessment of urban morphological structure parameters effects on meteorological fields in planetary boundary layer[J].China Environmental Science,2019,39(1):72-82.
Authors:SHEN Chong  SHEN Ao  TIAN Chun-yan  WEI Xiao-lin  LI Lei  WANG Ming-jie  CHEN Xun-lai  FAN Qi
Institution:1. School of Atmospheric Sciences/Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou 510275, China; 2. Meteorological Bureau of Shenzhen Municipality, Shenzhen 518040, China
Abstract:In this paper, the regional meteorological model WRF with urban canopy scheme has been used to study the impacts of urban morphological parameters on the meteorological fields in planetary boundary layer over the Shenzhen region (high population and building density city). The results from sensitivity experiments showed that the interception of heat in the urban canopy was enhanced in the daytime by the higher building height and density, and therefore the heat storage in the urban areas was also increased by about 6W/m2 and 9W/m2. Considering the effects of both shading and trapping by the urban canopy, the skin surface temperature was reduced by about 0.3℃ with the increased building height, and the skin surface temperature was increased by more than 0.6℃ in the daytime with the higher building density. In addition, there is a good consistency between the 2m temperature and the skin surface temperature. The wind speed was decreased by about 0.4m/s due to higher building height and 0.6m/s due to higher building density through the increased surface roughness. In the meantime, the nocturnal boundary layer was increased by about 30~40m due to higher building height and 20~30m due to higher building density at night through the enhancement of turbulent motion. On the contrary, the decreases of building height and density reduced the heat storage by 6~7.5W/m2 in the daytime, increased the 10m wind speed by about 0.3m/s and 0.4m/s, and decreased the nocturnal boundary layer height by about 30~50m and 10~30m.
Keywords:urban morphological structure  meteorological elements  WRF  urban canopy scheme  
本文献已被 CNKI 等数据库收录!
点击此处可从《中国环境科学》浏览原始摘要信息
点击此处可从《中国环境科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号