TY - JOUR
T1 - Ozone pollution around a coastal region of South China Sea
T2 - interaction between marine and continental air
AU - Wang, Hao
AU - Lyu, Xiaopu
AU - Guo, Hai
AU - Wang, Yu
AU - Zou, Shichun
AU - Ling, Zhenhao
AU - Wang, Xinming
AU - Jiang, Fei
AU - Zeren, Yangzong
AU - Pan, Wenzhuo
AU - Huang, Xiaobo
AU - Shen, Jin
N1 - Funding Information:
Acknowledgements. This project was supported by the Natural Science Foundation of China (grant no. 41275122), the Research Grants Council (RGC) of the Hong Kong Government of Special Administrative Region (PolyU5154/13E, PolyU152052/14E, PolyU152052/16E and CRF/C5004-15E), the Guangdong special fund for science and technology development (2017B020216007) and partly by the Hong Kong PolyU internal grant (G-SB63, 1-BBW4 and 4-ZZFW). The authors thank HKEPD for provision of the air quality and meteorological data at TC site and are grateful to Po On Commercial Association Wan Ho Kan Primary School at Tung Chung and the National Marine Environmental Monitoring Station at Wanshan Island for their generous support of the field study. Contributions to field measurements by Kalam Cheung, Dawei Wang, Bo Liu, Nan Wang, Jiamin Ou, Huanghuang Yan and Xiaoxin Fu are also highly appreciated. The authors also gratefully acknowledge the NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT transport and dispersion model and/or READY website (http://www.ready.noaa.gov) and Tao Wang’s group of the Hong Kong Polytechnic University for the provision of the average diurnal profiles of HONO at TC and HT.
Publisher Copyright:
© Author(s) 2018.
PY - 2018/3
Y1 - 2018/3
N2 - Marine atmosphere is usually considered to be a clean environment, but this study indicates that the near-coast waters of the South China Sea (SCS) suffer from even worse air quality than coastal cities. The analyses were based on concurrent field measurements of target air pollutants and meteorological parameters conducted at a suburban site (Tung Chung, TC) and a nearby marine site (Wan Shan, WS) from August to November 2013. The observations showed that the levels of primary air pollutants were significantly lower at WS than those at TC, while the ozone (O3) value was greater at WS. Higher O3 levels at WS were attributed to the weaker NO titration and higher O3 production rate because of stronger oxidative capacity of the atmosphere. However, O3 episodes were concurrently observed at both sites under certain meteorological conditions, such as tropical cyclones, continental anticyclones and sea-land breezes (SLBs). Driven by these synoptic systems and mesoscale recirculations, the interaction between continental and marine air masses profoundly changed the atmospheric composition and subsequently influenced the formation and redistribution of O3 in the coastal areas. When continental air intruded into marine atmosphere, the O3 pollution was magnified over the SCS, and the elevated O3 ( > g 100g ppbv) could overspread the sea boundary layer ∼ 8 times the area of Hong Kong. In some cases, the exaggerated O3 pollution over the SCS was recirculated to the coastal inshore by sea breeze, leading to aggravated O3 pollution in coastal cities. The findings are applicable to similar mesoscale environments around the world where the maritime atmosphere is potentially influenced by severe continental air pollution.
AB - Marine atmosphere is usually considered to be a clean environment, but this study indicates that the near-coast waters of the South China Sea (SCS) suffer from even worse air quality than coastal cities. The analyses were based on concurrent field measurements of target air pollutants and meteorological parameters conducted at a suburban site (Tung Chung, TC) and a nearby marine site (Wan Shan, WS) from August to November 2013. The observations showed that the levels of primary air pollutants were significantly lower at WS than those at TC, while the ozone (O3) value was greater at WS. Higher O3 levels at WS were attributed to the weaker NO titration and higher O3 production rate because of stronger oxidative capacity of the atmosphere. However, O3 episodes were concurrently observed at both sites under certain meteorological conditions, such as tropical cyclones, continental anticyclones and sea-land breezes (SLBs). Driven by these synoptic systems and mesoscale recirculations, the interaction between continental and marine air masses profoundly changed the atmospheric composition and subsequently influenced the formation and redistribution of O3 in the coastal areas. When continental air intruded into marine atmosphere, the O3 pollution was magnified over the SCS, and the elevated O3 ( > g 100g ppbv) could overspread the sea boundary layer ∼ 8 times the area of Hong Kong. In some cases, the exaggerated O3 pollution over the SCS was recirculated to the coastal inshore by sea breeze, leading to aggravated O3 pollution in coastal cities. The findings are applicable to similar mesoscale environments around the world where the maritime atmosphere is potentially influenced by severe continental air pollution.
UR - http://www.scopus.com/inward/record.url?scp=85044666511&partnerID=8YFLogxK
U2 - 10.5194/acp-18-4277-2018
DO - 10.5194/acp-18-4277-2018
M3 - Journal article
AN - SCOPUS:85044666511
SN - 1680-7316
VL - 18
SP - 4277
EP - 4295
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 6
ER -