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Influence of Southeast Asian biomass burning on ozone and carbon monoxide over subtropical Taiwan
Abstract Surface ozone (O3) and carbon monoxide (CO) mixing ratios were measured at Mei-Feng (24.05 °N, 120.10 °E, 2269 m above sea level) remote mountain site between March 2009 and September 2010 to investigate the impact of regional pollution on O3 and CO. The results showed that the maximum values of both O3 and CO were found in the springtime. Backward trajectory analysis, combined with MODIS fire spots suggested that the enhanced O3 and CO in springtime could be attributed to biomass burning (BB) activities over Southeast (SE) Asia. Thirteen BB events were identified by backward trajectory analysis, MODIS fires, NCEP weather data sets and CO concentrations. Good correlation between O3 and CO was found during the BB plumes. Using the linear regression, the slope (ΔO3/ΔCO) was calculated to be 0.18 ± 0.08 (mean ± 1σ). This value was in agreement with that of 0.2 observed over the west Pacific region during the TRACE-P campaign, but was higher than those (0.11–0.14) of Canadian and Siberian fires. Moreover, significant enhanced O3 productivity was also found in aged BB plumes and that mixed with urban emissions from SE coastal China. To assess the net influence of SE Asian BB, the air masses from SE Asia and SE China were divided in two groups: those that passed over the fire regions (PF) and those that did not (NP). The result showed that the maximum differences between PF and NP were estimated in March with 8 ppb for O3 and 45 ppb for CO, respectively, accounting for 23% of both CO and O3 levels at Mei-Feng. Although uncertainties existed in the estimations, the significant discrepancies of O3 and CO in the two air groups suggested the air pollutants emitted by SE Asian BB could be transported and influence the air quality over subtropical Taiwan in springtime.
Highlights ► We examine the spring-maximum of O3 and CO levels in subtropical Taiwan are attributed to Southeast Asian biomass burning. ► The average ΔO3/ΔCO ratio in fire plumes is 0.18 ± 0.08. ► Enhanced O3 production in aged fire plume and that mixed with urban emissions is found. ► The net influence of Southeast Asian biomass burning on both tropospheric O3 and CO was approximately 23% in March.
Influence of Southeast Asian biomass burning on ozone and carbon monoxide over subtropical Taiwan
Abstract Surface ozone (O3) and carbon monoxide (CO) mixing ratios were measured at Mei-Feng (24.05 °N, 120.10 °E, 2269 m above sea level) remote mountain site between March 2009 and September 2010 to investigate the impact of regional pollution on O3 and CO. The results showed that the maximum values of both O3 and CO were found in the springtime. Backward trajectory analysis, combined with MODIS fire spots suggested that the enhanced O3 and CO in springtime could be attributed to biomass burning (BB) activities over Southeast (SE) Asia. Thirteen BB events were identified by backward trajectory analysis, MODIS fires, NCEP weather data sets and CO concentrations. Good correlation between O3 and CO was found during the BB plumes. Using the linear regression, the slope (ΔO3/ΔCO) was calculated to be 0.18 ± 0.08 (mean ± 1σ). This value was in agreement with that of 0.2 observed over the west Pacific region during the TRACE-P campaign, but was higher than those (0.11–0.14) of Canadian and Siberian fires. Moreover, significant enhanced O3 productivity was also found in aged BB plumes and that mixed with urban emissions from SE coastal China. To assess the net influence of SE Asian BB, the air masses from SE Asia and SE China were divided in two groups: those that passed over the fire regions (PF) and those that did not (NP). The result showed that the maximum differences between PF and NP were estimated in March with 8 ppb for O3 and 45 ppb for CO, respectively, accounting for 23% of both CO and O3 levels at Mei-Feng. Although uncertainties existed in the estimations, the significant discrepancies of O3 and CO in the two air groups suggested the air pollutants emitted by SE Asian BB could be transported and influence the air quality over subtropical Taiwan in springtime.
Highlights ► We examine the spring-maximum of O3 and CO levels in subtropical Taiwan are attributed to Southeast Asian biomass burning. ► The average ΔO3/ΔCO ratio in fire plumes is 0.18 ± 0.08. ► Enhanced O3 production in aged fire plume and that mixed with urban emissions is found. ► The net influence of Southeast Asian biomass burning on both tropospheric O3 and CO was approximately 23% in March.
Influence of Southeast Asian biomass burning on ozone and carbon monoxide over subtropical Taiwan
Lin, Yu Chi (author) / Lin, Chuan Yao (author) / Lin, Po Hsiung (author) / Engling, Guenter (author) / Lin, Yen Ching (author) / Lan, Yung Yao (author) / June Chang, Chiung Wen (author) / Kuo, Tien Ho (author) / Hsu, Wei Ting (author) / Ting, Chia Chun (author)
Atmospheric Environment ; 64 ; 358-365
2012-09-17
8 pages
Article (Journal)
Electronic Resource
English
Biomass burning spatiotemporal variations over South and Southeast Asia
| Elsevier | 2020