Abstract

CMAQ was implemented in the central region of Saudi Arabia and the effect of simulating models using various chemical mechanisms on selected oxidants, nitrogen species, and O3 was investigated. CB05TUCL predicted OH, MEPX, and NOz about 7%, 7.7%, and 8% more than CB05E51 respectively; however, there was no observable difference in the O3 predictions. The differences in variations of SAPRC07 mechanism (SAPRC07TB, SAPRC07TC, and SAPRC07TIC) for all parameters were less than 1%. RACM2 produced the highest OH and H2O2 concentrations. RACM2 enhanced OH production in the range of 24% - 32% and H2O2 by 9% over other mechanisms; these are comparatively less than the findings of other studies. Similarly, CB05 produced over 40% more PAN concentration than CB05. Moreover, PAN concentrations produced by all mechanisms were very high compared to other studies. SAPRC07 produced approximately 3% more mean surface O3 concentration than RACM2 and approximately 10% more than CB05. RACM2 O3 predictions were higher than CB05 by 7%. The predicted O3 concentrations by CB05, RACM2, and SAPRC07 were 6%, 11%, and 15% more than the average observed concentrations, which indicate that closest predictions to the observed values were by CB05. This study concludes that there is a wide variation of mechanisms with respect to the predictions of oxidants and nitrogen compounds; however, less variation is noticed in predictions of O3. For any air pollution control strategies and photochemical modeling studies in the current region or in any other arid regions, the CB05 mechanism is recommended.

Highlights

  • Ozone (O3) is a secondary pollutant formed because of the reactions of its precursors: nitrogen oxides (NO + NO2 = NOx) and Volatile Organic Compounds (VOCs) in the presence of sunlight

  • The predicted O3 concentrations by CB05, RACM2, and SAPRC07 were 6%, 11%, and 15% more than the average observed concentrations, which indicate that closest predictions to the observed values were by CB05

  • The differences in the mean concentrations between the two Carbon Bond (CB) mechanisms were less than 1% except for OH, NOz, and MEPEX which had differences of 7%, 7.7% and 8% more than CB05TUCL respectively

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Summary

Introduction

Ozone (O3) is a secondary pollutant formed because of the reactions of its precursors: nitrogen oxides (NO + NO2 = NOx) and Volatile Organic Compounds (VOCs) in the presence of sunlight. The formation of O3 in the atmosphere can be understood through a combination of measurements (of O3 and its precursors) and model predictions. Measurements are generally limited in terms of space and time, so the atmospheric chemical transport models (ACTM) fill this gap. Several chemical mechanisms were developed for ACTM to address the issues associated with urban and rural O3 formation. Three of the more widely used mechanisms are the Carbon Bond (CB) [1], Regional Atmospheric Chemistry Mechanism (RACM) [2], and State Air Pollution Research Center (SAPRC) [3]

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