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Increasing surface ozone concentrations in the background atmosphere of southern China, 1994-2007

机译:1994-2007年中国南方本底大气中地表臭氧浓度增加

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摘要

Tropospheric ozone is of great importance with regard to air quality, atmospheric chemistry, and climate change. In this paper we report the first continuous record of surface ozone in the background atmosphere of South China. The data were obtained from 1994 to 2007 at a coastal site in Hong Kong, which is strongly influenced by the outflow of Asian continental air during the winter and the inflow of maritime air from the subtropics in the summer. Three methods are used to derive the rate of change in ozone. A linear fit to the 14-year record shows that the ozone concentration increased by 0.58 ppbv/yr, whereas comparing means in years 1994-2000 and 2001-2007 gives an increase of 0.87 ppbv/yr for a 7-year period. The ozone changes in air masses from various source regions are also examined. Using local wind and carbon monoxide (CO) data to filter out local influence, we find that ozone increased by 0.94 ppbv/yr from 1994- 2000 to 2001-2007 in air masses from Eastern China, with similar changes in the other two continent-influenced airmass groups, but no statistically significant change in the marine air. An examination of the nitrogen dioxide (NO₂) column obtained from GOME and SCIAMACHY reveals an increase in atmospheric NO₂ in China's three fastest developing coastal regions, whereas NO₂in other parts of Asia decreased during the same period, and no obvious trend over the main shipping routes in the South China Sea was indicated. Thus the observed increase in background ozone in Hong Kong is most likely due to the increased emissions of NO₂(and possibly volatile organic compounds (VOCs) as well) in the upwind coastal regions of mainland China. The CO data at Hok Tsui showed less definitive changes com-pared to the satellite NO 2 column. The increase in background ozone likely made a strong contribution (81%) to the rate of increase in "total ozone" at an urban site in Hong Kong, suggesting the need to consider distant sources when developing long-term strategies to mitigate local ozone pollution.
机译:对流层臭氧在空气质量,大气化学和气候变化方面非常重要。在本文中,我们报告了华南背景大气中地表臭氧的首次连续记录。这些数据是从1994年至2007年在香港的一个沿海站点获得的,该数据在很大程度上受到冬季冬季亚洲大陆空气的流出和夏季亚热​​带海洋空气的流入的影响。三种方法可用来推导臭氧的变化率。对14年记录的线性拟合显示,臭氧浓度增加了0.58 ppbv / yr,而比较1994-2000年和2001-2007年的臭氧浓度,则连续7年增加了0.87 ppbv / yr。还检查了来自各个源区域的空气质量中的臭氧变化。利用当地的风和一氧化碳(CO)数据过滤掉当地的影响,我们发现,从1994-2000年到2001-2007年,来自中国东部的空气质量中的臭氧增加了0.94 ppbv / yr,而在其他两个大陆,影响气团,但海洋空气没有统计学上的显着变化。对从GOME和SCIAMACHY获得的二氧化氮(NO 2)柱进行的检查显示,中国三个发展最快的沿海地区的大气NO 2有所增加,而亚洲其他地区的NO 2在同一时期有所减少,并且在主要运输路线上没有明显的趋势指示在南中国海。因此,在香港观察到的本底臭氧的增加很可能是由于中国大陆上风沿海地区的NO 2(以及可能的挥发性有机化合物(VOC))排放增加所致。与卫星NO 2柱相比,鹤咀的CO数据显示的确定性变化较小。背景臭氧的增加可能对香港市区内“总臭氧”的增加速度有很大的贡献(81%),这表明在制定长期战略以减轻当地臭氧污染时需要考虑遥远的来源。

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