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區域氣象環境與高臭氧之相關分析

Analysis of Local Circulation and High Ozone Generation

摘要


This study analyzsed the data gathered from the 17 new EPA stations and the CWB stations in the northern Taiwan area (Taipei) during the summer time (Jun.~Aug.) in 1993 and 1994. Also we analyzed the data gathered from the 14 new EPA stations and the CWB stations in the southern Taiwan area (Kao-hsiung) during the summer and fall (Jun.∼Nov.) in 1993 and 1994. We found that the ozone episodes usually happened during the summer time in the Taipei area, and the fall time in the Kao-hsiung area. The statistical High Ozone Days (HOD) is 64% in the Taipei area and 60% in the Kao-hsiung area. On the HOD, from the analysis we found that high hourly solar radiation (>55 min) and low cloud amount will lead to efficient photochemical reactions in Taipei and kao-hsiung area. Also the prevailing wind speed is weak (<4.0m/s) and the land-sea breeze ciruclation is significant. Before 8 AM, land breeze is dominant; during 8AM∼10AM, land breeze changes to sea breeze; after 10 AM, sea breeze is dominant, and reaches to the daily maximum at about 2PM. As other hourly ozone concentration character, at noon, the ozone value is creasing 8 times than that in the early morning and reaches to the daily maximum. In Taipei area, ozone episodes happened often in Shi-chih, Sung-shan and Tuu-chen, the respective statistic frequency is 33%, 32%, and 33%. While in Kao-hsiung area, the respective statistic frequency in Chiao-tou, Tso-ying, Ping-tong is 42%, 50% and 51%. The maximum ozone value can reach to be 215 ppb in Tuu-chen, and 206 ppb in Ping-tong, the position of these two stations is around the sea-breeze's down-wind zone.

並列摘要


This study analyzsed the data gathered from the 17 new EPA stations and the CWB stations in the northern Taiwan area (Taipei) during the summer time (Jun.~Aug.) in 1993 and 1994. Also we analyzed the data gathered from the 14 new EPA stations and the CWB stations in the southern Taiwan area (Kao-hsiung) during the summer and fall (Jun.∼Nov.) in 1993 and 1994. We found that the ozone episodes usually happened during the summer time in the Taipei area, and the fall time in the Kao-hsiung area. The statistical High Ozone Days (HOD) is 64% in the Taipei area and 60% in the Kao-hsiung area. On the HOD, from the analysis we found that high hourly solar radiation (>55 min) and low cloud amount will lead to efficient photochemical reactions in Taipei and kao-hsiung area. Also the prevailing wind speed is weak (<4.0m/s) and the land-sea breeze ciruclation is significant. Before 8 AM, land breeze is dominant; during 8AM∼10AM, land breeze changes to sea breeze; after 10 AM, sea breeze is dominant, and reaches to the daily maximum at about 2PM. As other hourly ozone concentration character, at noon, the ozone value is creasing 8 times than that in the early morning and reaches to the daily maximum. In Taipei area, ozone episodes happened often in Shi-chih, Sung-shan and Tuu-chen, the respective statistic frequency is 33%, 32%, and 33%. While in Kao-hsiung area, the respective statistic frequency in Chiao-tou, Tso-ying, Ping-tong is 42%, 50% and 51%. The maximum ozone value can reach to be 215 ppb in Tuu-chen, and 206 ppb in Ping-tong, the position of these two stations is around the sea-breeze's down-wind zone.

並列關鍵字

ozone episode land-see breeze

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