2015
DOI: 10.1016/j.atmosenv.2015.10.003
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SLCP co-control approach in East Asia: Tropospheric ozone reduction strategy by simultaneous reduction of NO x /NMVOC and methane

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Cited by 32 publications
(24 citation statements)
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“…They said that the rise in methane from May to September was due to rising temperatures during this period. Akimoto et al (2015) in the study of methane changes in East Asia witnessed seasonal changes in methane in their study area, which peaked in August and at least observed in February and March. Ganesan et al (2017) measured India's minimum methane concentration in winter and its peak concentration in August and July.…”
Section: Discussionmentioning
confidence: 99%
“…They said that the rise in methane from May to September was due to rising temperatures during this period. Akimoto et al (2015) in the study of methane changes in East Asia witnessed seasonal changes in methane in their study area, which peaked in August and at least observed in February and March. Ganesan et al (2017) measured India's minimum methane concentration in winter and its peak concentration in August and July.…”
Section: Discussionmentioning
confidence: 99%
“…The MIROC-AGCM fields were nudged toward the 6-hourly ERA-Interim reanalysis (Dee et al, 2011). The emission inventories used were obtained from the emission scenarios for the Greenhouse Gas and Air Pollution Interactions and Synergies (GAINS) model developed by the International Institute for Applied System Analysis (IIASA) (Klimont et al, 2009;Akimoto et al, 2015).…”
Section: Miroc Model Outputmentioning
confidence: 99%
“…Tropospheric ozone is a major air pollutant that can damage human skin and lungs, reduce agricultural output, and increase levels of premature mortality [1]. It is also one of the greenhouse gases that lead to a rise in the surface temperature by absorbing long-wave radiation energy at the surface of the Earth and re-releasing the energy [2,3]. Tropospheric ozone can be introduced directly from the stratosphere [4][5][6], or formed via the photochemical reactions of ozone precursors such as methane (CH 4 ), carbon monoxide (CO), nitrogen oxides (NO x ), and volatile organic compounds (VOCs) [7].…”
Section: Introductionmentioning
confidence: 99%