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DOI | 10.5194/acp-22-2351-2022 |
Enhanced summertime ozone and SOA from biogenic volatile organic compound (BVOC) emissions due to vegetation biomass variability during 1981-2018 in China | |
Cao, Jing; Situ, Shuping; Hao, Yufang; Xie, Shaodong; Li, Lingyu | |
发表日期 | 2022 |
ISSN | 1680-7316 |
EISSN | 1680-7324 |
起始页码 | 2351 |
结束页码 | 2364 |
卷号 | 22期号:4页码:14 |
英文摘要 | Coordinated control of fine particulate matter (PM2.5) and ozone (O-3) has become a new and urgent issue for China's air pollution control. Biogenic volatile organic compounds (BVOCs) are important precursors of O-3 and secondary organic aerosol (SOA) formation. China experienced a rapid increase in BVOC emissions as a result of increased vegetation biomass. We applied WRF-Chem3.8 coupling with MEGAN2.1 to conduct long-term simulations for impacts of BVOC emissions on O-3 and SOA during 1981-2018, using the emission factors extrapolated by localized emission rates and annual vegetation biomass. In summer 2018, BVOC emissions were 9.91 Tg (in June), which led to an average increase of 8.6 ppb (16.75 % of the total) in daily maximum 8 h (MDA8) O-3 concentration and 0.84 mu gm-3 (73.15 % of the total) in SOA over China. The highest contribution to O-3 is concentrated in the Great Khingan Mountains, Qinling Mountains, and most southern regions while in southern areas for SOA. Isoprene has the greatest contribution to O-3, while monoterpene has the largest SOA production. BVOC emissions have distinguished impacts in different regions. The Chengdu-Chongqing (CC) region has the highest O-3 and SOA generated by BVOCs, while the Beijing-Tianjin-Hebei (BTH) region has the lowest. From 1981 to 2018, the interannual variation of BVOC emissions caused by increasing leaf biomass resulted in O-3 concentration increasing by 7.38 % at an average rate of 0.11 ppb yr(-1) and SOA increasing by 39.30 % at an average rate of 0.008 mu gm-3 yr(-1). Due to the different changing trends of leaf biomass by region and vegetation type, O-3 and SOA show different interannual variations. The Fenwei Plain (FWP), Yangtze River Delta (YRD), and Pearl River Delta (PRD) regions have the most rapid O-3 increment, while the increasing rate of SOA in CC is the highest. BTH has the smallest enhancement in O-3 and SOA concentration. This study will help to recognize the impact of historical BVOC emissions on O-3 and SOA and further provide a reliable scientific basis for the precise prevention and control of air pollution in China. |
学科领域 | Environmental Sciences; Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000760569300001 |
来源期刊 | ATMOSPHERIC CHEMISTRY AND PHYSICS |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/273751 |
作者单位 | Qingdao University; Peking University |
推荐引用方式 GB/T 7714 | Cao, Jing,Situ, Shuping,Hao, Yufang,et al. Enhanced summertime ozone and SOA from biogenic volatile organic compound (BVOC) emissions due to vegetation biomass variability during 1981-2018 in China[J],2022,22(4):14. |
APA | Cao, Jing,Situ, Shuping,Hao, Yufang,Xie, Shaodong,&Li, Lingyu.(2022).Enhanced summertime ozone and SOA from biogenic volatile organic compound (BVOC) emissions due to vegetation biomass variability during 1981-2018 in China.ATMOSPHERIC CHEMISTRY AND PHYSICS,22(4),14. |
MLA | Cao, Jing,et al."Enhanced summertime ozone and SOA from biogenic volatile organic compound (BVOC) emissions due to vegetation biomass variability during 1981-2018 in China".ATMOSPHERIC CHEMISTRY AND PHYSICS 22.4(2022):14. |
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