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Published byVeronika Indradjaja Modified over 6 years ago
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Simulation of Ozone and PM in Southern Taiwan
Yee-Lin Wu and Der-Min Tsai Department of Environmental Engineering National Cheng Kung University Tainan, Taiwan
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Background: Monitoring sites
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Background:
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Background: PM10 seasonal variations
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Background: conc. of particulate matter
Sampling duration: Oct ~ Feb. 1999
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Background: conc. of particulate matter
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Objectives To evaluate the performance of Models-3/CMAQ for ozone and PM simulation in southern Taiwan
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Methods: emission Sparse Matrix Operator Kernel Emission modeling system ( SMOKE ) TEDS 4.2: SOx, NOx, CO, PM and VOCs point, area and mobile sources: emission inventory come from TEDS 4.2 using RADM mechanism to treat the VOCs temporal variations using measurement and TEDS biogenic: 7 types of land use in Taiwan based on BEIS II emission factors
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Results: Emission
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Methods: Models-3/CMAQ
Chemical mechanism: RADM2 Aerosol module: aero2 (RPM) Cloud: RADM Without plume in grid module Four domains simulation 15 layers of sigma layer Simulation duration: 1996/11/21~26
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Methods: Grid information
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Results: Concentrations compare with measurement data ( NanZi )
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Results: (simulation - observation)/observation
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Results: fine particle
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Results: fine particle
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Results: fine particle
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Results: fine particle
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Conclusions Models-3/CMAQ had been established for simulation of ozone and PM in Taiwan. Biogenic emissions are likely to be underestimated by using BEIS II and 7 type of land use in Taiwan
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Conclusions Simulation results:
Primary pollutant ( CO, NO ) concentrations agreed with measurement data fairly; NO2 concentration was in better agreement with measurement data. However, peak ozone concentration was significantly underestimated.
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Conclusions Simulation results:
Simulated concentrations of nitrate were greater than those of sulfate; however, the opposite was observed in the field. Simulated nitrate concentrations were more consistent with measured than those for sulfate. Diurnal variations of NO3- and HNO3 were similar between simulation and observation. However, the peak concentrations of HNO3 and NO3- were not in the same ranges.
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Acknowledgements We would like to thank Taipower and EPRI for supporting the project and to Prof. C. Wu for the meteorological simulation by MM5.
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