Journals / Atmospheric Pollution Research / 2016 / Cilt: 7 - Sayı: 3

Seasonal relationship between meteorological conditions and surface ozone in Korea based on an offline chemistry-climate model

Pages
385–392
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

Spring ozone levels tended to be elevated following maturephaseEl Nino winters, whereas elevated levels during summer and autumn followed La Ni ~ na winters

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Tropospheric ozone plays an important role in climate variation and air quality, and it has seen a dramaticrise in East Asia due to the region's rapid economic growth.
📊
Key Findings & Data:Increases in ozone were associated primarily with the westerly windanomaly during spring and with surface warming during the autumn and summer.
💡
Conclusion & Impact:Spring ozone levels tended to be elevated following maturephaseEl Nino winters, whereas elevated levels during summer and autumn followed La Ni ~ na winters
🔬Design:Modeling & Simulation
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Özet

Tropospheric ozone plays an important role in climate variation and air quality, and it has seen a dramaticrise in East Asia due to the region's rapid economic growth. The relationship between meteorologicalconditions and surface ozone in Korea varies seasonally, and to obtain a better understanding ofthis process, this study performed offline simulations using a climateechemistry model. The modelrepresented the observed annual cycle of surface ozone over East Asia well, including the spring/autumnpeaks and summer troughs. Increases in ozone were associated primarily with the westerly windanomaly during spring and with surface warming during the autumn and summer. Moreover, a decreasein ozone during the summer likely resulted from the transportation of ozone-depleted air masses byanomalous southeasterly winds. Reduced cloud cover increased ozone levels significantly during allseasons except winter. The relationship between the El Nino and Southern Oscillation and ozone con- ~centrations in Korea was also examined. Spring ozone levels tended to be elevated following maturephaseEl Nino winters, whereas elevated levels during summer and autumn followed La Ni ~ na winters

🔖

Cite This Article

WİE, J., MOON, B. K. (2016). Seasonal relationship between meteorological conditions and surface ozone in Korea based on an offline chemistry-climate model. Atmospheric Pollution Research, Cilt: 7 - Sayı: 3, 385–392. https://ajindex.com/articles/351505

References (1)

  1. Akimoto, H., 2003. Global air quality and pollution. Science 302, 1716e1719. Allen, R.J., Sherwood, S.C., Norris, J.R., Zender, C.S., 2012. Recent Northern Hemisphere tropical expansion primarily driven by black carbon and tropospheric ozone. Nature 485, 350e355. Bey, I., Jacob, D.J., Yantosca, R.M., Logan, J.A., Field, B.D., Fiore, A.M., Li, Q.B., Liu, H.G.Y., Mickley, L.J., Schultz, M.G., 2001. Global modeling of tropospheric chemistry with assimilated meteorology: model description and evaluation. J. Geophys. Research-Atmospheres 106, 23073e23095. http://dx.doi.org/ 10.1029/2001JD000807. Chang, C.C., Tsai, S.S., Ho, S.C., Yang, C.Y., 2005. Air pollution and hospital admissions for cardiovascular disease in Taipei, Taiwan. Environ. Res. 98, 114e119. Chang, C.P., Zhang, Y., Li, T., 2000. Interannual and interdecadal variations of East Asian summer monsoon and tropical Pacific SSTs. Part I: Roles of the subtropical ridge. J. Clim. 13, 4310e4325. Chatani, S., Sudo, K., 2011. Influences of the variation in inflow to East Asia on surface ozone over Japan during 1996e2005. Atmos. Chem. Phys. 11, 8745e8758. Choi, K.S., Kang, S.D., Kim, H.D., Wang, B., 2014. The spatio-temporal characteristics of total rainfall during September in South Korea according to the variation of ENSO. Clim. Dyn. 42, 1139e1154. Chou, C., Tu, J.Y., Yu, J.Y., 2003. Interannual variability of the western North Pacific summer monsoon: Differences between ENSO and non-ENSO years. J. Clim. 16, 2275e2287. Collins, W.D., Rasch, P.J., Boville, B.A., Hack, J.J., McCaa, J.R., Williamson, D.L., Briegleb, B.P., Bitz, C.M., Lin, S.J., Zhang, M.H., 2006. The formulation and atmospheric simulation of the community Atmosphere Model version 3 (CAM3). J. Clim. 19, 2144e2161. Cooper, O.R., Parrish, D.D., Stohl, A., Trainer, M., Nedelec, P., Thouret, V., Cammas, J.P., Oltmans, S.J., Johnson, B.J., Tarasick, D., Leblanc, T., McDermid, I.S., Jaffe, D., Gao, R., Stith, J., Ryerson, T., Aikin, K., Campos, T., Weinheimer, A., Avery, M.A., 2010. Increasing springtime ozone mixing ratios in the free troposphere over western North America. Nature 463, 344e348. Crutzen, P.J., 1974. Photochemical reactions initiated by and influencing ozone in unpolluted tropospheric air. Tellus 26, 47e57. Dentener, F., Stevenson, D., Cofala, J., Mechler, R., Amann, M., Bergamaschi, P., Raes, F., Derwent, R., 2005. The impact of air pollutant and methane emission controls on tropospheric ozone and radiative forcing: CTM calculations