A New Scheme for the Simulation of Microscale Flow and Dispersion in Urban Areas by Coupling Large-Eddy Simulation with Mesoscale Models
Autor: | Zhaoshun Zhang, Haifeng Li, Guixiang Cui |
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Rok vydání: | 2017 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Turbulence Mesoscale meteorology Mechanics Wind direction 01 natural sciences Wind speed 010305 fluids & plasmas Plume Physics::Fluid Dynamics 0103 physical sciences Turbulence kinetic energy Physics::Atmospheric and Oceanic Physics Geology Microscale chemistry 0105 earth and related environmental sciences Large eddy simulation |
Zdroj: | Boundary-Layer Meteorology. 167:145-170 |
ISSN: | 1573-1472 0006-8314 |
DOI: | 10.1007/s10546-017-0323-5 |
Popis: | A coupling scheme is proposed for the simulation of microscale flow and dispersion in which both the mesoscale field and small-scale turbulence are specified at the boundary of a microscale model. The small-scale turbulence is obtained individually in the inner and outer layers by the transformation of pre-computed databases, and then combined in a weighted sum. Validation of the results of a flow over a cluster of model buildings shows that the inner- and outer-layer transition height should be located in the roughness sublayer. Both the new scheme and the previous scheme are applied in the simulation of the flow over the central business district of Oklahoma City (a point source during intensive observation period 3 of the Joint Urban 2003 experimental campaign), with results showing that the wind speed is well predicted in the canopy layer. Compared with the previous scheme, the new scheme improves the prediction of the wind direction and turbulent kinetic energy (TKE) in the canopy layer. The flow field influences the scalar plume in two ways, i.e. the averaged flow field determines the advective flux and the TKE field determines the turbulent flux. Thus, the mean, root-mean-square and maximum of the concentration agree better with the observations with the new scheme. These results indicate that the new scheme is an effective means of simulating the complex flow and dispersion in urban canopies. |
Databáze: | OpenAIRE |
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