Variations of surface ozone concentration across the Klang Valley, Malaysia: Fid-Bau Portal

Variations of surface ozone concentration across the Klang Valley, Malaysia

Latif, Mohd Talib / Huey, Lim Shun / Juneng, Liew

Abstract Hourly air quality data covering the period 2004–2008 was obtained from the Air Quality Division, the Department of Environment (DOE) through long-term monitoring by Alam Sekitar Sdn. Bhd. (ASMA) were analysed to investigate the variations of surface ozone (O3) in the Klang Valley, Malaysia. A total of nine monitoring stations were selected for analysis in this study and the results show that there are distinct seasonal patterns in the surface O3 across the Klang Valley. A high surface O3 concentration is usually observed between January and April, while a low surface O3 concentration is found between June and August. Analysis of daily variations in surface O3 and the precursors – NO, NO2, CO, NMHC and UVb, indicate that the surface O3 photochemistry in this study area exhibits a positive response to the intensity and wavelength in UVb while being influenced by the concentration of NOx, particularly through tritration processes. Although results from our study suggested that NMHCs may influence the maximum O3 concentration, further investigation is required. Wind direction during different monsoons was found to influence the concentration of O3 around the Klang Valley. HYSPLIT back trajectories (−72 h) were used to indicate the air-mass transport patterns on days with high concentrations of surface O3 in the study area. Results show that 47% of the high O3 days was associated with the localized circulation. The remaining 32% and 22% were associated with mid-range and long-range transport across the South China Sea from the northeast.

Highlights ► We analyse ozone data from nine stations in Klang Valley, Malaysia. ► Surface O3 photochemistry exhibits a positive response to an increase in UVb. ► Surface O3 influences by NOx and wind directions. ► 47% of the high O3 days was associated with the localized circulation. ► Surface O3 also associated with mid-range and long-range transport.