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O 3 and fine particle pollution in China and regional air quality modeling Yuanhang Zhang College of Environmental Sciences Peking University Beijing 100871, China
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Outline O 3 in regions and high mountains PM 2.5 in regions Trends in Beijing and Hong Kong (PRD) Regional & global modeling
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Li Jiang E_Mei Mt Hai Nan Wu Dang Mt Wu Yi Mt Zhou Shan PKU_ BOGES Mt. Everest Beijing-Tianjing City Clusters (Mega City) Mega, large, middle, small cities/towns: connected through intensely economic activities Formed due to fast urbanization City-Clusters in eastern coast areas Pearl River Delta Yangtze River Delta Vehicle in Beijing Mt. Waliguan
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O 3 pollution in Beijing
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June 21-July 3, 2000 ) Spatial distribution of O 3 in Beijing area ( June 21-July 3, 2000 ) 8 hrs mean Maximun
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O 3 in PKU campus April, July and August
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Gaseous pollutants in Xinken (Rural area of Guangzhou)
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Aircraft PRD regional O 3 pollution High O 3 Conc.
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O 3 concentation in Yangtze Delta JiaXin JianHu LinAn SheShan ChangShu
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O 3 in Mt. Everest (From T. Zhu)
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O 3 in Waliguan: Gaw station From CAMS
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From Prof. Akimoto
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PM 2.5 concentrations in several regions and cities of China 2003,8 E_Mei Mt. 54 ug/m3 Wuyi Mt. 54 ug/m3
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PM 2.5 in fives stations in PRD Average during Oct 7-Nov 4, 2004 PM 2.5 /PM 10 CH 0.87 HZ 0.70 WQS0.69 UB* 0.78 Aircraft0.86
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Chemical speciation of PM 2.5 Main chemical compositions of PM 2.5 in several locations, ug/m 3 (Some data from joint project of PKU and Georgia Tech) SO 4 2- + NO 3 - + NH 4 + + OC: 60-70% Beijing: 95.5 ug/m 3
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Variation of light scattering and absorption coefficient in Guangzhou 300 61 0.83 Collaboration with MPI and IFT, Germany
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Climate effects of aerosol pollution Radiative forcing is negative: –25 Wm –2 TOA –100 Wm –2 BOA 25% integral daylight decrease of BOA solar flux 37% decrease of NO 2 photolysis rate SSA ( 0.87 ) GZ 0.83 Beijing 0.79 Lin-An 0.82 Guangzhou Collaboration with MPI and IFT, Germany
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Relationship between light absorption and OC/EC in Guangzhou b abs = 9.79 + 0.758*OC + 7.70*EC R 2 = 0.958 Urban from MPI Xinken EC : 70 - 80 % OC : 20 - 30 %
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Oxidative capacity in an increasing trend in Hong Kong O 3 +NO or O 3 : 1ppb/yr
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NO 2 O 3 +NO 2 O3O3 11 year Trend of O 3 in Taipei (Shaw Liu)
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Changes of AOD in Beijing 2001200220032004 Spring Summer Autumn Winter From Li et al.
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Changes of AOD in PRD Gray Haze Day 85 98 144 From Li et al.
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Long-range Trans-boundary Air Pollutants in Northeast Asia Participants: –China –Korea –Japan Focus: –Concentrations of S, N, O 3 and PM –Wet and dry depositions –Source and receptor relationship for sulfur In the second phase
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Monthly average of SO 2, NOx, O 3, sulfate, March 2002 case SO2 NOx SO 4 2- O3
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Source and receptor relationship for sulfur, March 2002 case, % Source budgetReceptor budget Very draft results
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Wang, Z.F of IAP GEATM development In operation SO 2, SO 4 2-, Dust, BC, Hg, etc. SO 2 Simulation SO 2 Stateline data Global Environmental Atmospheric Transport Model
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IMPACT,Chuang et al. 2002 GEATM Wang Z. F. IMPACT Chuang et al. 2002
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Net flux in each grid In-flowOut-flow
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Summary O 3 and fine particle concentration in China was high Trend? O 3 and AOD, in increasing PM 2.5 ? Regional & global modeling
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