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Boundary-Layer Meteorology

, Volume 118, Issue 3, pp 477–501 | Cite as

Vertical Structure of the Urban Boundary Layer over Marseille Under Sea-Breeze Conditions

  • Aude Lemonsu
  • Sophie Bastin
  • Valéry Masson
  • Philippe Drobinski
Article

Abstract

During the UBL-ESCOMPTE program (June–July 2001), intensive observations were performed in Marseille (France). In particular, a Doppler lidar, located in the north of the city, provided radial velocity measurements on a 6-km radius area in the lowest 3 km of the troposphere. Thus, it is well adapted to document the vertical structure of the atmosphere above complex terrain, notably in Marseille, which is bordered by the Mediterranean sea and framed by numerous massifs. The present study focuses on the last day of the intensive observation period 2 (26 June 2001), which is characterized by a weak synoptic pressure gradient favouring the development of thermal circulations. Under such conditions, a complex stratification of the atmosphere is observed. Three-dimensional numerical simulations, with the Méso-NH atmospheric model including the town energy balance (TEB) urban parameterization, are conducted over south-eastern France. A complete evaluation of the model outputs was already performed at both regional and city scales. Here, the 250-m resolution outputs describing the vertical structure of the atmosphere above the Marseille area are compared to the Doppler lidar data, for which the spatial resolution is comparable. This joint analysis underscores the consistency between the atmospheric boundary layer (ABL) observed by the Doppler lidar and that modelled by Méso-NH. The observations and simulations reveal the presence of a shallow sea breeze (SSB) superimposed on a deep sea breeze (DSB) above Marseille during daytime. Because of the step-like shape of the Marseille coastline, the SSB is organized in two branches of different directions, which converge above the city centre. The analysis of the 250-m wind fields shows evidence of the role of the local topography on the local dynamics. Indeed, the topography tends to reinforce the SSB while it weakens the DSB. The ABL is directly affected by the different sea-breeze circulations, while the urban effects appear to be negligible.

Keywords

Atmospheric boundary layer Doppler lidar Numerical simulation Sea breezes Topography 

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Copyright information

© Springer 2006

Authors and Affiliations

  • Aude Lemonsu
    • 2
  • Sophie Bastin
    • 1
  • Valéry Masson
    • 2
  • Philippe Drobinski
    • 1
  1. 1.Institut Pierre Simon Laplace/Service d’AéronomieUniversité Pierre & Marie CurieParis Cedex 05France
  2. 2.Météo-FranceCentre National de Recherches MétéorologiquesCedexFrance

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