Process analysis and sensitivity study of regional ozone formation over the Pearl River Delta, China, during the PRIDE-PRD2004 campaign using the Community Multiscale Air Quality modeling system
Item
Title (Dublin Core)
Process analysis and sensitivity study of regional ozone formation over the Pearl River Delta, China, during the PRIDE-PRD2004 campaign using the Community Multiscale Air Quality modeling system
Description (Dublin Core)
In this study, the Community Multiscale Air Quality (CMAQ) modeling system is used to simulate the ozone (O<sub>3</sub>) episodes during the Program of Regional Integrated Experiments of Air Quality over the Pearl River Delta, China, in October 2004 (PRIDE-PRD2004). The simulation suggests that O<sub>3</sub> pollution is a regional phenomenon in the Pearl River Delta (PRD). Elevated O<sub>3</sub> levels often occurred in the southwestern inland PRD, Pearl River estuary (PRE), and southern coastal areas during the 1-month field campaign. Three evolution patterns of simulated surface O<sub>3</sub> are summarized based on different near-ground flow conditions. More than 75% of days featured interactions between weak synoptic forcing and local sea-land circulation. Integrated process rate (IPR) analysis shows that photochemical production is a dominant contributor to O<sub>3</sub> enhancement from 09:00 to 15:00 local standard time in the atmospheric boundary layer over most areas with elevated O<sub>3</sub> occurrence in the mid-afternoon. The simulated ozone production efficiency is 2–8 O<sub>3</sub> molecules per NO<sub>x</sub> molecule oxidized in areas with high O<sub>3</sub> chemical production. Precursors of O<sub>3</sub> originating from different source regions in the central PRD are mixed during the course of transport to downwind rural areas during nighttime and early morning, where they then contribute to the daytime O<sub>3</sub> photochemical production. The sea-land circulation plays an important role on the regional O<sub>3</sub> formation and distribution over PRD. Sensitivity studies suggest that O<sub>3</sub> formation is volatile-organic-compound-limited in the central inland PRD, PRE, and surrounding coastal areas with less chemical aging (NO<sub>x</sub>/NO<sub>y</sub>>0.6), but is NO<sub>x</sub>-limited in the rural southwestern PRD with aged air (NO<sub>x</sub>/NO<sub>y</sub><0.3).
Creator (Dublin Core)
Wang, X.
Zhang, Y.
Hu, Y.
Zhou, W.
Lu, K.
Zhong, L.
Zeng, L.
Shao, M.
Hu, M.
Russell, A. G.
Date (Dublin Core)
2018-01-15
Type (Dublin Core)
info:eu-repo/semantics/Text
Format (Dublin Core)
info:eu-repo/semantics/application/pdf
Identifier (Dublin Core)
10.5194/acp-10-4423-2010
https://acp.copernicus.org/articles/10/4423/2010/
Source (Dublin Core)
eISSN: 1680-7324
Language (Dublin Core)
eng
Relation (Dublin Core)
info:eu-repo/grantAgreement/EC/FP7/212095
Rights (Dublin Core)
info:eu-repo/semantics/openAccess
