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


Estimating micrometeorological inputs for modeling dispersion in urban areas during stable conditions
Institution:1. Université de Lille Nord de France, F-59000 Lille, France;2. EMDouai, CE, F-59508 Douai, France;3. TERA-Environnement, 628 rue Charles De Gaulle, 38926 Crolles, France;1. University of California, Riverside, CA 92521, USA;2. U.S. Environmental Protection Agency, Office of Research and Development, National Exposure Research Laboratory, Research Triangle Park, NC 27711, USA;3. U.S. Environmental Protection Agency, Office of Research and Development, National Risk Management Research Laboratory, Research Triangle Park, NC 27711, USA;1. Department of Mechanical Engineering, University of California, Riverside, CA 92521, USA;2. Atmospheric Modeling and Analysis Division, National Exposure Research Laboratory, MD-81, U.S. Environmental Protection Agency, Research Triangle Park, NC 27711, USA
Abstract:We examine the performance of three methods to estimate the surface friction velocity and the Monin–Obukhov (MO) length in stable conditions. Estimates from these methods are compared with measurements made at two urban sites: the Wilmington site located in the middle of an urban area, and the VTMX site located on a sloping, smooth area in Salt Lake City. The first method uses the mean wind at a single height (Single U or SU), the second uses the wind speed at a single level and the temperature difference between two levels (U delta T or UDT), and the third method uses two levels of wind speed and temperature (delta U delta T or DUDT). The performance of the SU and UDT methods in estimating u* are comparable. The SU method yields better estimates of the MO length than the UDT method does. The DUDT method performs poorly in estimating both u* and L. The major conclusions of this study are that (1) measurements of mean winds and temperatures at one or two levels at an urban location can provide adequate estimates of micrometeorological variables required in modeling dispersion in the stable boundary layer, and (2) methods based on using differences in temperatures and velocities between two levels can provide unreliable estimates of these variables because these differences can be overwhelmed by inevitable uncertainties in the measurement of mean variables.
Keywords:
本文献已被 ScienceDirect 等数据库收录!
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