Boundary-Layer Meteorology

, Volume 113, Issue 1, pp 111–158

Simulation of Meteorological Fields Within and Above Urban and Rural Canopies with a Mesoscale Model

  • Sylvain Dupont
  • Tanya L. Otte
  • Jason K. S. Ching
Article

DOI: 10.1023/B:BOUN.0000037327.19159.ac

Cite this article as:
Dupont, S., Otte, T.L. & Ching, J.K.S. Boundary-Layer Meteorology (2004) 113: 111. doi:10.1023/B:BOUN.0000037327.19159.ac

Abstract

Accurate simulation of air quality at neighbourhood scales (on order of 1-km horizontal grid spacing) requires detailed meteorological fields inside the roughness sub-layer (RSL). Since the assumptions of the roughness approach, used by most of the mesoscale models, are unsatisfactory at this scale, a detailed urban and rural canopy parameterisation, called DA-SM2-U, is developed inside the Penn State/NCAR Mesoscale Model (MM5) to simulate the meteorological fields within and above the urban and rural canopies. DA-SM2-U uses the drag-force approach to represent the dynamic and turbulent effects of the buildings and vegetation, and a modified version of the soil model SM2-U, called SM2-U(3D), to represent the thermodynamic effects of the canopy elements. The turbulence length scale is also modified inside the canopies. SM2-U(3D) assesses the sensible and latent heat fluxes from rural and urban surfaces in each of the computational layers inside the canopies by considering the shadowing effect, the radiative trapping by the street canyons, and the storage heat flux by the artificial surfaces. DA-SM2-U is tested during one simulated day above the city of Philadelphia, U.S.A. It is shown that DA-SM2-U is capable of simulating the important features observed in the urban and rural RSL, as seen in the vertical profiles of the shear stress, turbulent kinetic energy budget components, eddy diffusivity, potential air temperature, and specific humidity. Within the canopies, DA-SM2-U simulates the decrease of the wind speed inside the dense canopies, the skirting of the flow around the canopy blocks, warmer air inside the vegetation canopy than above open areas during the night and conversely during the day, and constantly warmer air inside the urban canopy. The comparison with measurements shows that the surface air temperature above rural and urban areas is better simulated by DA-SM2-U than by the `standard version' of MM5.

Eddy diffusivity Energy budget Mesoscale models Rural and urban canopies Urban boundary layer 

Copyright information

© Kluwer Academic Publishers 2004

Authors and Affiliations

  • Sylvain Dupont
    • 1
  • Tanya L. Otte
    • 1
  • Jason K. S. Ching
    • 1
  1. 1.NOAA Air Resources Laboratory, Atmospheric Sciences Modeling DivisionUSA

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