Parameterization of the urban energy budget with the submesoscale soil model

被引:62
作者
Dupont, Sylvain
Mestayer, Patrice G.
机构
[1] INRA, EPHYSE, F-33883 Villenave Dornon, France
[2] Ecole Cent Nantes, CNRS, UMR 6598, Lab Mecan Fluides, Nantes, France
关键词
D O I
10.1175/JAM2417.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The thermal component of the Soil Model for Submesoscales, Urbanized Version (SM2-U), is described. SM2-U is an extension on a physical basis of the rural Interactions between Soil, Biosphere, and Atmosphere (ISBA) soil model to urban areas. It evaluates the turbulent energy, moisture, and radiative fluxes at the urban canopy-atmosphere interface to provide lower boundary conditions of high-resolution mesoscale models. Unlike previous urban canopy schemes, SM2-U integrates in a simple way the physical processes inside the urban canopy: the building wall influence is integrated in the pavement temperature equation, allowing the model to compute directly the energy budget of street canyons. The SM2-U model is evaluated on the Marseille, France, city-center energy-budget components measured during the field experiments to constrain models of atmospheric pollution and transport of emissions [Experience sur Site pour Contraindre les Modeles de Pollution Atmospherique et de Transport d'Emissions (ESCOMPTE)] urban boundary layer (UBL) campaign (June-July 2001). The observed behavior of net radiation and heat fluxes is reproduced by SM2-U with a high level of quality, demonstrating that the influence of building walls may be well modeled by modifying the pavement temperature equation.
引用
收藏
页码:1744 / 1765
页数:22
相关论文
共 62 条
[31]   Intercomparisons of experimental convective heat transfer coefficients and mass transfer coefficients of urban surfaces [J].
Hagishima, A ;
Tanimoto, J ;
Narita, K .
BOUNDARY-LAYER METEOROLOGY, 2005, 117 (03) :551-576
[32]   Scalar Fluxes from Urban Street Canyons Part II: Model [J].
Ian N. Harman ;
Janet F. Barlow ;
Stephen E. Belcher .
Boundary-Layer Meteorology, 2004, 113 (3) :387-410
[33]   Review of some basic characteristics of the atmospheric surface layer [J].
Hogstrom, U .
BOUNDARY-LAYER METEOROLOGY, 1996, 78 (3-4) :215-246
[34]   Thermal effects of urban canyon structure on the nocturnal heat island: Numerical experiment using a mesoscale model coupled with an urban canopy model [J].
Kusaka, H ;
Kimura, F .
JOURNAL OF APPLIED METEOROLOGY, 2004, 43 (12) :1899-1910
[35]   A simple single-layer urban canopy model for atmospheric models: Comparison with multi-layer and slab models [J].
Kusaka, H ;
Kondo, H ;
Kikegawa, Y ;
Kimura, F .
BOUNDARY-LAYER METEOROLOGY, 2001, 101 (03) :329-358
[36]   Derivation of the relationship between the Obukhov stability parameter and the bulk Richardson number for flux-profile studies [J].
Launiainen, J .
BOUNDARY-LAYER METEOROLOGY, 1995, 76 (1-2) :165-179
[37]  
Lemonsu A, 2004, J APPL METEOROL, V43, P312, DOI 10.1175/1520-0450(2004)043<0312:MTSEBO>2.0.CO
[38]  
2
[39]  
LEMONSU A, 2003, THESIS U TOULOUSE 3
[40]  
LONG N, 2003, P 5 INT C URB CLIM L, V1, P95