Analyzing the basic features of different complex terrain flows by means of a Doppler Sodar and a numerical model: Some implications for air pollution problems

SummaryA variety of programmes and field experiments were carried out in order to develop and evaluate models of transport and diffusion of pollutants in complex terrain areas. As part of this programme, in this study, we have focused our interest on analyzing the basic features of different flow fields and thermal structures developed in a complex area and their relation to air pollution problems. The area is located in the province of Barcelona (in the northeast of Spain) close to a wide industrial zone, thus a pollutant flux could affect this region. In order to carry out the main purpose of this study we have analysed data from a Doppler Sodar (FAS 64) and a network of near surface meteorological and air quality stations. In addition, different dynamical simulations given by a numerical mesoscale model (MM5) are also analyzed. The results show that the main flow fields and thermal structures generated in this area are: sea breeze, slope drainage winds, channelling winds created by terrain constrictions and cool-air accumulation in low-lying regions. This last structure, developed specially in winter time, gives rise to stagnant cold air masses and strong thermic inversions, with average lapse rate of −4 degrees on 100 m, which contribute to increase air pollution concentration, especially SO2. Hourly and daily averaged SO2 concentration can be higher than 350 and 138 µg m−3 respectively. In addition, as “La Plana” is located not far from the Mediterranean Sea, during summertime the sea breeze arrives into this zone via its southern entrance, thereby reaching the whole area. The arrival of the sea breeze in to “La Plana”, which advects pollutants from the nearby industrial area, is the main cause of some of these pollutants, especially ozone and its precursors, attaining high concentrations during afternoon hours. The contribution of the sea breeze is variable, but could represent between a 25% to a 30% of its total value.

[1]  T. McKee,et al.  The Role of Valley Geometry and Energy Budget in the Formation of Nocturnal Valley Winds , 1989 .

[2]  G. Grell,et al.  A description of the fifth-generation Penn State/NCAR Mesoscale Model (MM5) , 1994 .

[3]  H. Lenschow,et al.  Probing the atmospheric boundary layer , 1986 .

[4]  S. Galmarini,et al.  Evolution of Nitrogen Oxide Chemistry in the Nocturnal Boundary Layer , 1997 .

[5]  R. Stull An Introduction to Boundary Layer Meteorology , 1988 .

[6]  Günther Zängl,et al.  An Improved Method for Computing Horizontal Diffusion in a Sigma-Coordinate Model and Its Application to Simulations over Mountainous Topography , 2002 .

[7]  J. Garratt The Atmospheric Boundary Layer , 1992 .

[8]  W. Junkermann,et al.  Assessing the meteorological conditions of a deep Italian Alpine valley system by means of a measuring campaign and simulations with two models during a summer smog episode , 2001 .

[9]  C. Whiteman Mountain Meteorology: Fundamentals and Applications , 2000 .

[10]  W. Clements,et al.  Mean Structure of the Nocturnal Drainage Flow in a Deep Valley , 1989 .

[11]  John S. Kain,et al.  Convective parameterization for mesoscale models : The Kain-Fritsch Scheme , 1993 .

[12]  W. Neff,et al.  Observations of complex terrain flows using acoustic sounders: Drainage flow structure and evolution , 1988 .

[13]  J. Bossert,et al.  A numerical investigation of mechanisms affecting drainage flows in highly Complex Terrain , 1995 .

[14]  S. Belcher,et al.  Tethered Balloon Observations Of The Nocturnal Stable Boundary Layer In A Valley , 2000 .

[15]  B. Lamb,et al.  Improving ozone modeling in regions of complex terrain using observational nudging in a prognostic meteorological model , 2000 .

[16]  I. Vergeiner,et al.  Valley winds and slope winds — Observations and elementary thoughts , 1987 .

[17]  I. Troen,et al.  A simple model of the atmospheric boundary layer; sensitivity to surface evaporation , 1986 .

[18]  F. Beyrich,et al.  Some aspects of determining the stable boundary layer depth from sodar data , 1993 .