Identification and Interpretation of Representative Ozone Distributions in Association with the Sea Breeze from Different Synoptic Winds over the Coastal Urban Area in Korea

• Published in: Journal of the Air & Waste Management Association (1995) 2007-12, Vol.57 (12), p.1480-1488
• Main Authors: Hwang, Mi-Kyoung, Kim, Yoo-Keun, Oh, In-Bo, Lee, Hwa Woon, Kim, Cheol-Hee
• Format: Article
• Language: English
• Subjects: Air Pollutants - analysis; Air Pollutants - chemistry; Air Pollution - analysis; Applied sciences; Atmospheric circulation; Atmospheric ozone; Case studies; Cities; Data analysis; Environmental aspects; Environmental Monitoring; Exact sciences and technology; Korea; Meteorology; Observations; Ozone - analysis; Pollution; Principal components analysis; Properties; Quality standards; Research methodology; Sea breeze; Simulation; Suburban areas; Time Factors; Wind
• ISSN: 1096-2247; 2162-2906
• DOI: 10.3155/1047-3289.57.12.1480

To aid the studies of long-term impact assessment of cumulative ozone (O 3 ) exposures, the representative 8-hr O 3 pollution patterns have been identified over the Greater Seoul Area (GSA) in Korea. Principal component analysis and two-stage clustering techniques were used to identify the representative O 3 patterns, and numerical and observational analyses were also used to interpret the identified horizontal distribution patterns. The results yielded three major O 3 distribution patterns, and each of the three patterns was found to have strong correlations with local and synoptic meteorological conditions over the GSA. For example, pattern 1, accounting for 46% of O 3 concentration distributions, mostly occurred under relatively weak westerly synoptic winds. The predominant features of this pattern were infrequent high O 3 levels but a distinct gradient of O 3 concentration from the western coastal area to the eastern inland area that was mainly induced by the local sea breeze. Pattern 2, accounting for 31% of O 3 concentration distributions, was found with higher O 3 levels in the western coastal area but lower in the eastern inland area. This is due to the modified sea breeze under the relatively stronger easterly opposing synoptic wind, affecting the high O 3 occurrence in the western coastal area only. However, pattern 3, accounting for 21% of O 3 concentration distributions, showed significantly higher O 3 concentrations over the whole GSA mainly due to the retarded and slow-moving sea-breeze front under the weak opposing synoptic flow. Modeling study also indicated that local and synoptic meteorological processes play a major role in determining the high O 3 concentration distribution patterns over the GSA.