论文

城市下垫面对北京冬季气象要素影响的模拟研究

  • 程宸 ,
  • 王晓云 ,
  • 苗世光 ,
  • 王颖
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  • 南京信息工程大学遥感学院, 南京 210044;2. 中国气象局气象探测中心, 北京 100081;3. 中国气象局北京城市气象研究所, 北京 100089;4. 北京市气候中心, 北京 100089

收稿日期: 2012-12-28

  网络出版日期: 2014-08-28

基金资助

国家重点基础研究发展计划973项目(2010CB428506);公益性行业(气象)科研专项(GYHY201106032,GYHY200906026);国家自然科学基金项目(41175015)

Study of Different Methods for Simulating the Impact of Urban Surface on Meteorological Elements in Beijing in Winter

  • CHENG Chen ,
  • WANG Xiaoyun ,
  • MIAO Shiguang ,
  • WANG Ying
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  • School of Remote Sensing, Nanjing University of Information Science & Technology, Nanjing 210044, China;2. Meteorological Observation Center, CMA, Beijing 100081, China;3. Institute of Urban Meteorology, CMA, Beijing 100089, China;4. Beijing Municipal Climate Center, Beijing 100089, China

Received date: 2012-12-28

  Online published: 2014-08-28

摘要

首先总结和分析了气象站观测的2012年1月北京地区主要天气过程和月平均物理量分布特征,然后利用中尺度天气预报模式WRF(Weather Research and Forecasting Model),通过个例模拟平均和平均场模拟两种方法分别模拟了1月北京新、旧城市土地利用状况下月平均2 m温度、2 m比湿和10 m风速;将模拟结果与观测结果验证之后,对比分析了两种模拟方法反映城市发展对冬季月平均气象要素的影响特征。结果表明,两种模拟方法均具有较好的模拟效果,对城区月平均2 m温度、比湿的模拟命中率在70%以上,10 m风速超过60%,且二者对研究区月平均物理量的模拟在空间分布特征和日变化规律是一致的,平均场对2 m气温的模拟效果好于对湿度和风速的模拟;城市下垫面发展对北京地区冬季月平均气象条件影响显著,两种方法在模拟城市发展对月平均气象条件影响方面有较好的一致性,个例模拟平均方法能得到极端影响状况,平均场模拟方法局限性在于无法得到极端影响状况和降水模拟。

本文引用格式

程宸 , 王晓云 , 苗世光 , 王颖 . 城市下垫面对北京冬季气象要素影响的模拟研究[J]. 高原气象, 2014 , 33(4) : 1045 -1056 . DOI: 10.7522/j.issn.1000-0534.2013.00062

Abstract

This paper focuses on two different methods for simulating the impact of urban surface development on monthly averaged meteorological elements in Beijing winter. After analyzing the major weather process and distribution characteristics of month mean meteorological elements in Beijing in January 2012, using WRF/BEP modeling system, the month mean 10 m wind speed, 2 m air temperature and 2 m humidity were simulated by the cases-averaged method and the mean-field method. Then the results of two methods under new and old land use conditions are evaluated against the observation. At last, the analysis of affect caused by urban development and the comparison of two different methods for reflecting this affect are carried out. The results show that: Both methods have good simulation results. Hite rate of air temperature and specific humidity is higher than 70% and the wind speed is more than 60%. The spatial distribution of the characteristics of month-averaged meteorological elements and diurnal variation simulated by two methods are consistent. Urbanization slightly decreases the specific humidity and wind speed in Beijing but increases the air temperature. And the impact of urbanization simulated by two approaches also have the same trend. The cases-averaged method not only reflects the average impact of urban development but also gets the extreme impact of a month. The mean-field method may not get the extreme impact conditions and precipitation simulation.

参考文献

[1]李卓仑, 王乃昂, 轧靖, 等. 近40年兰州城市气候季节性变化与城市发展[J]. 高原气象, 2007, 26(3): 586-592.
[2]周雅清, 任国玉. 城市化对华北地区最高、最低气温和日较差变化趋势的影响[J]. 高原气象, 2009, 28(5): 1158-1166.
[3]苗世光, 王晓云, 蒋维楣, 等. 城市小区规划大气环境影响评估研究[J]. 高原气象, 2007, 26(1): 92-97.
[4]李江林, 陈玉春, 吕世华, 等. 利用RAMS模式对山谷城市冬季局地风场的数值模拟[J]. 高原气象, 2009, 28(6): 1250-1259.
[5]郑祚芳, 高华, 王在文, 等. 北京地区降水空间分布及城市效应分析[J]. 高原气象, 2014, 33(2): 522-529, doi: 10.7522/j.issn.1000-0534.2012.00193.
[6]黄鹤, 李英华, 韩素芹, 等. 天津城市边界层湍流统计特征[J]. 高原气象, 2011, 30(6): 1481-1487.
[7]蒋维楣, 苗世光, 张宁, 等. 城市气象与边界层数值模拟研究[J]. 地球科学进展, 2010, 25(5): 463-473.
[8]王颖, 张镭, 胡菊, 等. WRF模式对山谷城市边界层模拟能力的检验及地面气象特征分析[J]. 高原气象, 2010, 29(6): 1397-1407.
[9]ChuanYao Lin, Fei Chen, Huang J C, et al. Urban heat island effect and its impact on boundary layer development and land-sea circulation over northern Taiwan[J]. Atmos Environ, 2008, 42(22): 5635-5649.
[10]苗世光, 王晓云, 孙桂平, 等. 青岛奥帆赛高分辨率数值模式系统研制与应用[J]. 应用气象学报, 2009, 20(3): 379-379.
[11]李欣, 杨修群, 汤剑平, 等. WRF/NCAR模拟的夏季长三角城市群区域多城市热岛和地表能量平衡[J]. 气象科学, 2011, 31(4): 441-450.
[12]苗世光, Chen Fei, 李青春, 等. 北京城市化对夏季大气边界层结构及降水的月平均影响[J]. 地球物理学报, 2001, 53(7): 1580-1593.
[13]Xi Lu, Kim C C, Teng Yao, et al. Effects of urbanization on the land sea breeze circulation over PRD region in winter[J]. Inter J Climatol, 2010, 30: 1089-1104.
[14]周荣卫, 何小凤, 苗世光, 等. 北京地区大气环流型及气候特征[J]. 气候变化研究进展, 2010, 6(5): 1673-1719.
[15]北京市统计局, 国家统计局北京调查总队. 北京统计年鉴2011[M]. 北京: 中国统计出版社, 2011: 9.
[16]Miao Shiguang, Chen Fei, Margaret A L, et al. An observational and modeling study of characteristics of urban heat island and boundary layer structures in Beijing[J]. J Appl Meteor Climatol, 2009, 48(3): 484-501.
[17]Skamarock W C, Klemp J B, Dudhia J, et al. A description of the Advanced Research WRF Version 3[Z]. NCAR Tech Note TN-475+STR, 2008: 113.
[18]张亦洲, 苗世光, 戴永久, 等. 北京夏季晴天边界层特征及城市下垫面对海风影响的数值模拟[J]. 地球物理学报, 2013, 56(8): 2558-2573.
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