首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >NITROGEN OXIDES AND OZONE PRODUCTION IN THE NORTH ATLANTIC MARINE BOUNDARY LAYER
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NITROGEN OXIDES AND OZONE PRODUCTION IN THE NORTH ATLANTIC MARINE BOUNDARY LAYER

机译:北大西洋海洋边界层中的氮氧化物和臭氧产生

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摘要

Measurements of reactive nitrogen gases (NO, NO2, NOy), as well as related chemical (O-3, CO, aerosol black carbon, radon, selected nonmethane hydrocarbons) and meteorological parameters were made on board the R/V Malcolm Baldridge prior to and subsequent to the 1992 ASTEX (Atlantic Stratocumulus Transition Experiment) in the North Atlantic Ocean during June and July 1992. Results showed indications of well-defined plumes from North America and Europe from both chemistry and back trajectory data. Elevated ozone concentrations were also observed in airmasses from uninhabited continental regions. Chemical and meteorological data were incorporated into a simple photochemical model in which ozone destruction predominated over generation. The principal reaction leading to ozone destruction was O(D-1) + H2O --> 2OH. [References: 46]
机译:在R / V Malcolm Baldridge船上之前,对反应性氮气(NO,NO2,NOy)以及相关化学物质(O-3,CO,气溶胶黑碳,ra,选定的非甲烷碳氢化合物)和气象参数进行了测量。以及1992年6月和7月在北大西洋的1992年ASTEX(大西洋平流层过渡实验)之后。结果表明,从化学和后向轨迹数据来看,北美和欧洲的羽状羽均清晰可见。在无人居住的大陆区域的气团中也观察到臭氧浓度升高。化学和气象数据被整合到一个简单的光化学模型中,在该模型中,臭氧破坏在生成过程中占主导地位。导致臭氧破坏的主要反应是O(D-1)+ H2O-> 2OH。 [参考:46]

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