Abstract

Atmospheric dispersion calculations are made using the HYSPLIT Particle Dispersion Model for studying the transport and dispersion of air-borne releases from point elevated sources in the Mississippi Gulf coastal region. Simulations are performed separately with three meteorological data sets having different spatial and temporal resolution for a typical summer period in 1–3 June 2006 representing a weak synoptic condition. The first two data are the NCEP global and regional analyses (FNL, EDAS) while the third is a meso-scale simulation generated using the Weather Research and Forecasting model with nested domains at a fine resolution of 4 km. The meso-scale model results show significant temporal and spatial variations in the meteorological fields as a result of the combined influences of the land-sea breeze circulation, the large scale flow field and diurnal alteration in the mixing depth across the coast. The model predicted SO2 concentrations showed that the trajectory and the concentration distribution varied in the three cases of input data. While calculations with FNL data show an overall higher correlation, there is a significant positive bias during daytime and negative bias during night time. Calculations with EDAS fields are significantly below the observations during both daytime and night time though plume behavior follows the coastal circulation. The diurnal plume behavior and its distribution are better simulated using the mesoscale WRF meteorological fields in the coastal environment suggesting its suitability for pollution dispersion impact assessment in the local scale. Results of different cases of simulation, comparison with observations, correlation and bias in each case are presented.

Highlights

  • Increasing urbanization, industrial growth and population expansion in coastal areas necessitates accurate air pollution dispersion estimates

  • This study explores the impact of using three different meteorological inputs on atmospheric transport and dispersion model solutions calculated by the Hybrid Single Particle Lagrangian Integrated trajectory model (HYSPLIT) model

  • A chemically non-active tracer is released in HYSLIT from four sites in the coastal zone of MS, with mass corresponding to reported emissions of SO2

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Summary

Introduction

Increasing urbanization, industrial growth and population expansion in coastal areas necessitates accurate air pollution dispersion estimates. Pollutant plumes in the coastal zones are influenced by development of meso-scale sea breeze circulations as a result of differential heating of the land and water surfaces [1,2]. Differential land-sea temperatures and the incidence of local circulations initiate development of internal boundary layer (IBL), which has a critical effect on dispersion [3,4]. These local effects need to be accounted in the coastal dispersion simulation for realistic estimations of pollutant concentrations. Numerous studies show the spatial and temporal resolution of meteorological data is an important factor in accurate estimation of plume trajectories and concentration [5,6]. Nasstrom and Pace reported in 1998 that higher resolution meteorological data lead to improvement in meso-scale dispersion through better representation of flow features [7]

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