TY - JOUR
T1 - Area, mobile, and point source contributions to ground level ozone
T2 - A summer simulation across the continental USA
AU - Tao, Zhining
AU - Larson, Susan M.
AU - Williams, Allen
AU - Caughey, Michael
AU - Wuebbles, Donald J.
N1 - Funding Information:
The authors thank Dr. Xinzhong Liang of Illinois State Water Survey (ISWS) for providing the RCM results, Dr. Ho-Chun Huang of ISWS for helpful discussions of SAQM, and the Critical Research Initiative Program of University of Illinois at Urbana-Champaign (UIUC) for funding support. We sincerely acknowledge the National Center for Supercomputing Applications (NCSA) of UIUC for its computer support.
PY - 2005/3
Y1 - 2005/3
N2 - In this study, we assessed how much ground level O 3 originated from area, mobile, and point sources in the presence of biogenic emissions. We simulated ground level O 3 formation over a three-month period (June-August, 1995) across the continental US, using the procedure for factor separation (FS) to calculate our source contribution. The modeling system includes Sparse Matrix Operator Kernel Emissions (SMOKE), an emissions model, meteorological data from a regional climate model, and SAQM, a 3-D chemistry-transport air quality model. The FS technique is applied to quantify the pure impact from an individual source category as well as the additional impact due to the synergy among source categories. In performing this type of source contribution, it is important to note that the synergy among source categories may sometimes actually suppress O 3 formation in comparison with the sum of pure contribution from the individual source category. In such a case, a negative source contribution is assigned to this interaction. Our simulation results indicate that this suppression does occur and that pure and synergistic contributions vary over time and space. The full potential of each source category in O 3 formation (the pure contribution) is not achieved when emissions from the other source categories are accounted for, implying that control of emissions from one source category could increase the potential of emissions from another source category to produce O 3.
AB - In this study, we assessed how much ground level O 3 originated from area, mobile, and point sources in the presence of biogenic emissions. We simulated ground level O 3 formation over a three-month period (June-August, 1995) across the continental US, using the procedure for factor separation (FS) to calculate our source contribution. The modeling system includes Sparse Matrix Operator Kernel Emissions (SMOKE), an emissions model, meteorological data from a regional climate model, and SAQM, a 3-D chemistry-transport air quality model. The FS technique is applied to quantify the pure impact from an individual source category as well as the additional impact due to the synergy among source categories. In performing this type of source contribution, it is important to note that the synergy among source categories may sometimes actually suppress O 3 formation in comparison with the sum of pure contribution from the individual source category. In such a case, a negative source contribution is assigned to this interaction. Our simulation results indicate that this suppression does occur and that pure and synergistic contributions vary over time and space. The full potential of each source category in O 3 formation (the pure contribution) is not achieved when emissions from the other source categories are accounted for, implying that control of emissions from one source category could increase the potential of emissions from another source category to produce O 3.
KW - Anthropogenic inventory
KW - Factor separation
KW - Photochemical model
KW - Synergy
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U2 - 10.1016/j.atmosenv.2004.12.001
DO - 10.1016/j.atmosenv.2004.12.001
M3 - Article
AN - SCOPUS:14944358216
SN - 1352-2310
VL - 39
SP - 1869
EP - 1877
JO - Atmospheric Environment
JF - Atmospheric Environment
IS - 10
ER -