The atmospheric chemical process was simulated using the Carbon Bond 4 (CB-4) model, the aqueous-phase chemistry in Regional Acid Deposition Model and the thermodynamic equilibrium relation of aerosols with the emission inventories of the Emission Database for Global Atmospheric Research, the database of China and South Korea and the Mesoscale Model version 2 (MM5) meteorological fields to examine the spatial distributions of the acidic pollutant concentrations in East Asia for the case of the long-lasting Yellow Sand event in April 1998. The present models simulate quite well the observed general trend and the diurnal variation of concentrations of gaseous pollutants, especially for O₃ concentration. However, the model underestimates SO₂ and NO<SUB>x</SUB> concentration but overestimates O₃ concentration largely due to uncertainty in NO<SUB>x</SUB> and VOC emissions. It is found that the simulated gaseous pollutants such as SO₂, NO<SUB>x</SUB> , and NH₃ are not transported far away from the source regions but show significant diurnal variations of their concentrations. However, the daily variations of the concentrations are not significant due to invariant emission rates. On the other hand, concentrations of the transformed pollutants including SO²?₄, NH₄?, and NO?₃ are found to have significant daily variations but little diurnal variations. The model-estimated deposition indicates that dry deposition is largely contributed by gaseous pollutants while wet deposition of pollutants is mainly contributed by the transformed pollutants.<BR> ⓒ 2002 Elsevier Science Ltd. All rights reserved.
Abstract<BR>1. Introduction<BR>2. Model description<BR>3. Gaseous pollutant emissions<BR>4. Results<BR>5. Summary and conclusion<BR>Acknowledgements<BR>References<BR>
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