Comparison between the atmospheric boundary layer in Paris and its rural suburbs during the ECLAP experiment

• Published in: Atmospheric environment (1994) 1999-03, Vol.33 (6), p.979-994
• Main Authors: Dupont, E., Menut, L., Carissimo, B., Pelon, J., Flamant, P.
• Format: Article
• Language: English
• Subjects: Convection, turbulence, diffusion. Boundary layer structure and dynamics; Convective boundary layer; Earth, ocean, space; Exact sciences and technology; External geophysics; Lidar; Meteorology; Nocturnal boundary layer; Sodar; Urban boundary layer; Urban effects
• ISSN: 1352-2310; 1873-2844
• DOI: 10.1016/S1352-2310(98)00216-7

The ECLAP experiment has been performed during the winter of 1995 in order to study the influence of the urban area of Paris on the vertical structure and diurnal evolution of the atmospheric boundary layer, in situations favourable to intense urban heat island and pollution increase. One urban site and one rural site have been instrumented with sodars, lidars and surface measurements. Additional radiosondes, 100 m masts and Eiffel Tower data were also collected. This paper gives a general overview of this experiment, and presents results of the analysis of four selected days, characterized by various wind directions and temperature inversion strengths. This analysis, which consists in a comparison between data obtained in the two sites, has been focused on three parameters of importance to the ABL dynamics: the standard deviation of vertical velocity, the surface sensible heat flux, and the boundary layer height. The vertical component of turbulence is shown to be enhanced by the urban area, the amplitude of this effect strongly depending on the meteorological situation. The sensible heat flux in Paris is generally found larger than in the rural suburbs. The most frequent differences range from 25–65 W m -2, corresponding to relative differences of 20–60%. The difference of unstable boundary layer height between both sites are most of the time less than 100 m. However, sodar and temperature data show that the urban influence is enhanced during night-time and transitions between stable and unstable regimes.