TY - JOUR
T1 - Comprehensive study of emission source contributions for tropospheric ozone formation over East Asia
AU - Itahashi, Syuichi
AU - Hayami, Hiroshi
AU - Uno, Itsushi
N1 - Funding Information:
This work was supported in part by Grant-in-Aid for Scientific Research 25220101 from the Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan. The authors would like to thank three anonymous reviewers for their helpful comments. The authors are grateful to EANET and JMA for compiling and providing the measurement data of various air pollutants and meteorolog ical conditions. The observation data of EANET are available at http://www. eanet.asia/product/index.html, and those of JMA are available at http:// www.data.jma.go.jp/obd/stats/data/ mdrr/index.html.
Publisher Copyright:
© 2014. American Geophysical Union. All Rights Reserved.
PY - 2015/1/16
Y1 - 2015/1/16
N2 - Emission source contributions of tropospheric ozone (O3) were comprehensively investigated by using the higher-order decoupled direct method (HDDM) for sensitivity analysis and the ozone source apportionment technology (OSAT) for mass balance analysis in the comprehensive air-quality model with extensions (CAMx). The response of O to emissions reductions at various levels in mainland China, Korea, and Japan were estimated and compared with results calculated by the brute force method (BFM) where one model parameter is varied at a time. Emissions were assessed at three receptor sites in Japan that experienced severe pollution events in May 2009. For emissions from China, HDDM assessed O3 response with a bias of only up to 3 ppbv (a relative error of 4.5%) even for a 50% reduction but failed to assess a more extreme reduction. OSAT was reasonably accurate at 100% reduction, with a −4 ppbv (−7%) bias, but was less accurate at moderate ranges of reduction (∼50-70%). For emissions from Korea and Japan, HDDM captured the nonlinear response at all receptor sites and at all reduction levels to within 1% in all but one case; however, the bias of OSAT increased with the increasing reduction of emissions. One possible reason for this is that OSAT does not account for NO titration. To address this, a term for potential ozone (PO; O3and NO2 together) was introduced. Using of PO instead of O3 improved the performance of OSAT, especially for emissions reductions from Korea and Japan. The proposed approach with PO refined the OSAT results and did not degrade HDDM performance.
AB - Emission source contributions of tropospheric ozone (O3) were comprehensively investigated by using the higher-order decoupled direct method (HDDM) for sensitivity analysis and the ozone source apportionment technology (OSAT) for mass balance analysis in the comprehensive air-quality model with extensions (CAMx). The response of O to emissions reductions at various levels in mainland China, Korea, and Japan were estimated and compared with results calculated by the brute force method (BFM) where one model parameter is varied at a time. Emissions were assessed at three receptor sites in Japan that experienced severe pollution events in May 2009. For emissions from China, HDDM assessed O3 response with a bias of only up to 3 ppbv (a relative error of 4.5%) even for a 50% reduction but failed to assess a more extreme reduction. OSAT was reasonably accurate at 100% reduction, with a −4 ppbv (−7%) bias, but was less accurate at moderate ranges of reduction (∼50-70%). For emissions from Korea and Japan, HDDM captured the nonlinear response at all receptor sites and at all reduction levels to within 1% in all but one case; however, the bias of OSAT increased with the increasing reduction of emissions. One possible reason for this is that OSAT does not account for NO titration. To address this, a term for potential ozone (PO; O3and NO2 together) was introduced. Using of PO instead of O3 improved the performance of OSAT, especially for emissions reductions from Korea and Japan. The proposed approach with PO refined the OSAT results and did not degrade HDDM performance.
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U2 - 10.1002/2014JD022117
DO - 10.1002/2014JD022117
M3 - Article
AN - SCOPUS:84921963149
SN - 0148-0227
VL - 120
SP - 331
EP - 358
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
IS - 1
ER -