Journal
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 124, Issue 22, Pages 12340-12355Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2019JD030833
Keywords
ozone pollution; atmospheric dynamics; photochemical reactions; South China; WRF-Chem
Categories
Funding
- Research Grants Council of the Hong Kong Special Administrative Region (SAR) via Theme-Based Research Scheme (TRS) [T24-504/l 7-N]
- Research Grants Council of the Hong Kong Special Administrative Region (SAR) via Collaborative Research Fund [CRF/C5004-15E]
- Research Grants Council of the Hong Kong Special Administrative Region (SAR) via General Research Fund [PolyU 152052/14E, PolyU 152052/16E]
- Guangzhou Science and Technology Project [201604016053]
- Major Project of Industry-University-Research Collaborative Innovation in Guangzhou [2016201604030082]
- Public Policy Research Funding Scheme from Policy Innovation and Coordination Office of the Hong Kong Special Administrative Region Government [2017. A6.094.17D]
- Hong Kong Polytechnic University PhD scholarships (Project RUJA)
Ask authors/readers for more resources
Pearl River Estuary (PRE) has been recognized as one of the key areas in South China experiencing severe air pollution. To understand the photochemical pollution over PRE, intensive measurements of O-3 and its precursors were simultaneously conducted at a suburban site on the east bank of PRE (Tung Chung, TC) in Hong Kong and a rural site on the west bank (Qi'ao Island, QAI) in Zhuhai from 25 September to 29 November 2016. Three and sixteen O-3 episode days (days with the maximum hourly O-3 higher than 100 ppbv) were captured at TC and QAI, respectively. On the three days when O-3 episodes occurred at TC, QAI also suffered from O-3 episodes, which were all associated with tropical cyclones (typhoons). As a downwind site of PRE when northwesterly winds prevailed, TC displayed a higher maximum hourly O-3 than QAI on these three days. In contrast, the other thirteen episodes that solely occurred at QAI were generally under northeasterly winds, which brought more coastal air to TC and led to lower levels of O-3 at this site. In addition, the stronger titration of the locally emitted NO to O-3 also accounted for the lower O-3 at TC on these days. The simulations by Weather Research and Forecasting coupled with Chemistry model indicated that the interactions of synoptic winds and mesoscale breezes led to relatively weak winds and long residence time for air pollutants over the PRE, thereby air pollution accumulation. This provided the likelihood of intensive chemical productions of O-3 over PRE, with the production rates even higher than those in the surrounding land areas. As such, it was concluded that PRE was a pool of O-3, where atmospheric dynamics caused the accumulation of air pollutants and subsequently intensive photochemical reactions. The findings in this study may also apply to the other estuaries connecting terrestrial and marine systems over the world.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available