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1. Introduction
Surface ozone (O3) is harmful to humans [1] and ecosystems [2] at elevated concentrations, whereas O3 present in the upper troposphere acts as a greenhouse gas [1,3]. It is produced by the photochemical reaction of directly emitted nitrogen oxide precursors (NOx = NO + NO2) and volatile organic compounds (VOCs). Long-range transport of tropospheric O3 is possible such that it can reach the United States (U.S.) from East Asia [4,5,6,7,8,9,10,11,12,13,14,15]. In the 2000s, major East Asian countries began actively regulating air pollutants. South Korea and Japan have been enforcing stringent regulations on NOx emissions since the early 2000s [16,17,18]. In China, NOx emissions have also been on a downward trend since mid-2010s due to tougher restrictions on automobile emissions.
The O3 formation mechanism is based on the O3–NOx–VOC photochemical reaction chain, identified as either NOx-limited or NOx-saturated (VOC-limited) depending on the VOC/NOx ratio, and is relevant to O3 reduction policies focused on the NOx or VOC emission control priority. At high VOC/NOx ratios, O3 production is NOx-limited, and at low VOC/NOx ratios, the production is VOC-limited [19,20,21]. On the global scale, O3 production is largely dominated by the NOx-limited regime, though heavily polluted urban/metropolitan areas with high NOx emissions are frequently under the NOx-saturated condition [21,22]. NOx reductions could lead to decreasing ambient O3 under the NOx-limited regime as NOx emission reductions reduce the NO2 photolysis related to primary production of free oxygen atoms reacting with O2 into O3. Under the VOC-limited regime, a reduction in NOx emissions has resulted in increased O3 [20] due to weakened NO + O3 titration. Thus, as NOx emissions decline, O3 levels will continue to increase until the regime shifts to NOx-limited. Thus, surface O3 does not respond to a linear reduction in NOx.
Numerous O3 studies have been carried out to identify the characteristics of its changing trends and precursors in East Asia, in which the focus has been on high-emission areas, including...
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Details
; Lim-Seok, Chang 2 ; Jaffe, Daniel A 3
; Bak, Juseon 1
; Liu, Xiong 4
; Gonzalo González Abad 4
; Hyun-Young, Jo 1 ; Yu-Jin, Jo 5 ; Lee, Jae-Bum 2 ; Cheol-Hee, Kim 6
1 Institute of Environmental Studies, Pusan National University, Busan 46241, Korea;
2 Climate & Air Quality Research Department, National Institute of Environmental Research, Incheon 22689, Korea;
3 School of STEM, University of Washington Bothell, Bothell, WA 98011, USA;
4 Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA;
5 Department of Atmospheric Sciences, Pusan National University, Busan 46241, Korea;
6 Institute of Environmental Studies, Pusan National University, Busan 46241, Korea;




