globalchange  > 气候变化事实与影响
DOI: 10.1016/j.atmosenv.2015.04.015
Scopus记录号: 2-s2.0-84927626891
论文题名:
Source characterization of carbon monoxide and ozone over the Northwestern Pacific in summer 2012
作者: Park K; , Rhee T; S
刊名: Atmospheric Environment
ISSN: 0168-2563
EISSN: 1573-515X
出版年: 2015
卷: 111
起始页码: 151
结束页码: 160
语种: 英语
英文关键词: Carbon monoxide ; Global chemical transport model ; Marine boundary layer ; Ozone ; Source composition
Scopus关键词: Airships ; Boundary layers ; Carbon ; Carbon monoxide ; Chemical analysis ; Ozone ; Photochemical reactions ; Poles ; Ships ; Troposphere ; Upper atmosphere ; Anthropogenic emissions ; Chemical transport models ; Long range transport ; Lowermost stratosphere ; Marine boundary layers ; Source characteristics ; Source characterization ; Source composition ; Ozone layer ; carbon monoxide ; ozone ; atmospheric pollution ; boundary layer ; carbon monoxide ; emission ; long range transport ; ozone ; pollutant source ; pollutant transport ; Southern Hemisphere ; stratosphere ; troposphere ; Article ; Asia ; biomass ; Europe ; human ; North America ; priority journal ; Russian Federation ; stratosphere ; summer ; troposphere ; Bering Sea ; Korea ; Pacific Ocean ; Pacific Ocean (Northwest) ; Siberia ; Vindula arsinoe
Scopus学科分类: Environmental Science: Water Science and Technology ; Earth and Planetary Sciences: Earth-Surface Processes ; Environmental Science: Environmental Chemistry
英文摘要: Carbon monoxide (CO) and ozone (O3) were continuously measured in the marine boundary layer of the East Sea, the Northwestern Pacific, and the Bering Sea onboard R/V Araon in the second halves of July and September of 2012, as a part of the SHIpborne Pole-to-Pole Observations (SHIPPO) program. Depending on the characteristics of each section of the cruise track, up to 66ppbv and 17ppbv of CO and O3 variability were observed, respectively. The O3/CO ratio suggests that O3 was dominantly produced by photochemical reactions in the troposphere, although in the northern sections of the cruise track, the ratio likely suggests vertical transport from the free troposphere or the lowermost stratosphere. To analyze the source characteristics and the transport of both trace gases, a tagging technique in a 3-D global chemical transport model (Model for OZone And Related chemical Tracers-4; MOZART-4) was applied. The model reproduced the observations fairly well, and the technique enabled us to characterize the source regions and composition of the observed CO. Anthropogenic emissions from Northeastern Asian countries appeared to be substantial sources of the CO in the southern sections, and biomass burning in Siberia was an important source of the CO observed in the northern sections of the cruise track. Long-range transport of anthropogenic CO emissions was distinct over the Bering Sea, where the comparable contributions from North America, Northeast Asia, and Europe were identified. Low CO events driven by southern hemispheric invasion were encountered at the southern coast of the Korean peninsula and in the North Pacific at ~50N latitude. The model pointed to a noticeable contribution from the open ocean in the Southern Hemisphere for these events. © 2015 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/81762
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作者单位: Division of Polar Ocean Environment, Korea Polar Research Institute, Incheon, South Korea

Recommended Citation:
Park K,, Rhee T,S. Source characterization of carbon monoxide and ozone over the Northwestern Pacific in summer 2012[J]. Atmospheric Environment,2015-01-01,111
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