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CityFlux perfluorocarbon tracer experiments

机译:Cityflux全氟碳轨迹实验

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In June 2006, two perfluorocarbon tracer experiments were conducted in central Manchester UK as part of the CityFlux campaign. The main aim was to investigate vertical dispersion in an urban area during convective conditions, but dispersion mechanisms within the street network were also studied. Paired receptors were used in most cases where one receptor was located at ground level and one at roof level. One receptor was located on the roof of Portland Tower which is an 80 m high building in central Manchester. Source receptor distances in the two experiments varied between 120 and 600 m. The results reveal that maximum concentration was sometimes found at roof level rather than at ground level implying the effectiveness of convective forces on dispersion. The degree of vertical dispersion was found to be dependent on source receptor distance as well as on building height in proximity to the release site. Evidence of flow channelling in a street canyon was also found. Both a Gaussian profile and a street network model were applied and the results show that the urban topography may lead to highly effective flow channelling which therefore may be a very important dispersion mechanism should the right meteorological conditions prevail. The experimental results from this campaign have also been compared with a simple urban dispersion model that was developed during the DAPPLE framework and show good agreement with this. The results presented here are some of the first published regarding vertical dispersion. More tracer experiments are needed in order to further characterise vertical concentration profiles and their dependence on, for instance, atmospheric stability. The impact of urban topography on pollutant dispersion is important to focus on in future tracer experiments in order to improve performance of models as well as for our understanding of the relationship between air quality and public health.
机译:2006年6月,作为CityFlux运动的一部分,在曼彻斯特英国中部进行了两次全氟碳传递实验。主要目的是在对流条件下调查城市地区的垂直分散,但还研究了街道网络内的分散机制。在大多数病例中使用配对的受体,其中一个受体位于地面水平和屋顶水平的一个受体。一位受体位于波特兰塔屋顶,是曼彻斯特中部的80米高建筑。两个实验中的源极受体距离在120和600米之间变化。结果表明,最大浓度有时在屋顶水平上发现,而不是在地面上发现,这意味着对流力对分散的有效性。发现垂直分散的程度取决于源极受体距离以及在释放位点附近的建筑物高度。还发现了街道峡谷流动窜流的证据。应用高斯型材和街道网络模型,结果表明,城市地貌可能导致高效的流动窜流,因此如果普遍的气象条件普遍存在,因此可能是一个非常重要的分散机制。这项运动的实验结果也与一个简单的城市分散模型进行了比较,这些模型是在Dapple框架期间开发的,并与此表现出良好的一致意见。这里提出的结果是关于垂直分散的第一个发布。需要更多的示踪剂实验,以进一步表征垂直浓度曲线及其对例如大气稳定性的依赖性。城市地貌对污染物分散的影响对于未来的示踪实验很重要,以提高模型的表现,以及我们对空气质量与公共卫生之间关系的理解。

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