CANYON GEOMETRY, THE URBAN FABRIC AND NOCTURNAL COOLING: A SIMULATION APPROACH

A simulation model for surface cooling in urban street canyons under calm conditions is described, based upon a simplified energy budget for the canyon facets containing only the net longwave and substrate heat flux densities. The former term is evaluated from the canyon radiation budget model of Arnfield (1976), the latter by numerically approximating the Fourier heat conduction equation. Equilibrium temperatures evolve through the nocturnal period for specified canyon and incoming longwave irradiance characteristics. Numerical experiments conducted with the model show that canyon geometry alone exerts a significant effect on cooling rates and, hence, on heat island intensity. Construction materials and internal building climate control tend to enhance spatial variations in nocturnal temperatures. The effects of wall thickness, sky radiance distribution and cloud cover also are investigated. Results show qualitative and quantitative correspondences with previous field and scale-model studies. Sources of ...

[1]  Timothy R. Oke,et al.  Urban heat island dynamics in Montreal and Vancouver , 1975 .

[2]  Kohji Yamashita,et al.  On relationships between heat island and sky view factor in the cities of Tama River basin, Japan , 1986 .

[3]  J. Voogt Validation of an urban canyon radiation model for nocturnal long-wave radiative fluxes and the effect of surface geometry on cooling in urban canyons , 1989 .

[4]  T. Oke Canyon geometry and the nocturnal urban heat island: Comparison of scale model and field observations , 1981 .

[5]  T. Oke,et al.  Wind, temperature and stability conditions in an east-west oriented urban canyon , 1988 .

[6]  A. Arnfield Estimation of diffuse irradiance on sloping, obstructed surfaces: An error analysis , 1982 .

[7]  W. Brutsaert On a derivable formula for long-wave radiation from clear skies , 1975 .

[8]  Ray D. Jackson,et al.  Thermal radiation from the atmosphere , 1969 .

[9]  A. Arnfield AN APPROACH TO THE ESTIMATION OF THE SURFACE RADIATIVE PROPERTIES AND RADIATION BUDGETS OF CITIES , 1982 .

[10]  A. Arnfield VALIDATION OF AN ESTIMATION MODEL FOR URBAN SURFACE ALBEDO , 1988 .

[11]  T. Oke The energetic basis of the urban heat island , 1982 .

[12]  W. Swinbank Long‐wave radiation from clear skies , 1963 .

[13]  Fowler Spencer Duckworth,et al.  The effect of cities upon horizontal and vertical temperature gradients , 1954 .

[14]  Heinz Reuter Forecasting Minimum Temperatures , 1951 .

[15]  J. Mattsson,et al.  Canyon geometry, street temperatures and urban heat island in malmö, sweden , 1985 .

[16]  Evaluation of empirical expressions for the estimation of hourly and daily totals of atmospheric longwave emission under all sky conditions , 1979 .

[17]  T. Oke,et al.  Long-wave radiative flux divergence and nocturnal cooling of the urban atmosphere , 1976 .

[18]  Timothy R. Oke,et al.  The distinction between canopy and boundary‐layer urban heat islands , 1976 .

[19]  T. Oke,et al.  Validation of an urban canyon radiation model for nocturnal long-wave fluxes , 1991 .