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

内陆丘陵河谷地区小风条件下的大气扩散模拟研究
引用本文:朱好,蔡旭晖,张宏升,康凌,陈家宜.内陆丘陵河谷地区小风条件下的大气扩散模拟研究[J].环境科学学报,2011,31(3):613-623.
作者姓名:朱好  蔡旭晖  张宏升  康凌  陈家宜
作者单位:1. 北京大学物理学院大气与海洋科学系,北京,100871
2. 北京大学环境科学与工程学院环境科学系,北京,100871
基金项目:国家自然科学基金(No. 41075005);国家重点基础研究发展规划(973)项目(No. 2010CB428501);国家高技术研究发展计划(No. 2006AA06A306);财政部/科技部公益性行业(气象)科研专项(No. GYHY201006014)
摘    要:针对湖南中部丘陵河谷地区的气象特点,开展了小风条件下大气扩散的数值模拟研究,并与示踪实验结果进行比较.模拟采用美国EPA推荐的非稳态拉格朗日高斯烟团模式CALPUFF,以加密的地面气象观测资料、边界层垂直廓线观测资料和铁塔多层湍流观测资料作为模拟气象场的输入.中等风速和小风条件下的模拟结果表明:模式对地表类型及资料的分...

关 键 词:大气扩散  CALPUFF模式  示踪实验  小风  丘陵河谷
收稿时间:6/10/2010 8:13:13 PM
修稿时间:9/27/2010 3:46:24 PM

Atmospheric dispersion simulation in low wind conditions in inland hills and valleys
ZHU Hao,CAI Xuhui,ZHANG Hongsheng,KANG Ling and CHEN Jiayi.Atmospheric dispersion simulation in low wind conditions in inland hills and valleys[J].Acta Scientiae Circumstantiae,2011,31(3):613-623.
Authors:ZHU Hao  CAI Xuhui  ZHANG Hongsheng  KANG Ling and CHEN Jiayi
Institution:Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871,Department of Environmental Sciences, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871,Department of Environmental Sciences, College of Environmental Sciences and Engineering, Peking University, Beijing 100871 and Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871
Abstract:The atmospheric dispersion under conditions with moderate and low winds was simulated for the hill and valley area in the centre of Hunan province. The non-steady-state Lagrangian Gaussian puff model CALPUFF recommended by USEPA was used in the simulation. The inputs of the meteorological model included the intensive observations of surface wind and temperature, profiles of wind and temperature in the boundary-layer, and the multi-layer turbulence data from the tower. Results showed that the model was sensitive to the categories and resolution of land use data. Simulated results were compared with those of the tracer experiments. It is seen that the near field concentration simulated by the default micrometeorological scheme was significantly lower than that observed in the tracer experiment. This is partly because the default land use category and the corresponding surface parameters in the model cannot represent the actual surface conditions in the simulated area. When utilizing the direct measurements of turbulence, the modeled results were greatly improved. Modification was made for land use data, geophysical parameters and the parameterization scheme of the turbulent velocities of the model, based on the actual underlying surface features and the measured turbulence data. The simulated results of the modified scheme were in good agreement with the measured values, and were comparable with those modeled with the direct measurements of turbulence profiles. These facts show the effectiveness and the necessity of the modification.
Keywords:atmospheric dispersion  CALPUFF model  tracer experiment  low wind  hills and valley
本文献已被 万方数据 等数据库收录!
点击此处可从《环境科学学报》浏览原始摘要信息
点击此处可从《环境科学学报》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