Airborne measurements of gas and particle pollutants during CAREBeijing-2008
-
Published:2014-01-09
Issue:1
Volume:14
Page:301-316
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Zhang W., Zhu T.ORCID, Yang W., Bai Z., Sun Y. L., Xu Y., Yin B., Zhao X.
Abstract
Abstract. Measurements of gaseous pollutants – including ozone (O3), sulfur dioxide (SO2), nitrogen oxides (NOX = NO + NO2), carbon monoxide (CO), particle number concentrations (5.6–560 nm and 0.47–30 μm) – and meteorological parameters (T, RH, P) were conducted during the Campaigns of Air Quality Research in Beijing and Surrounding Regions in 2008 (CAREBeijing-2008), from 27 August through 13 October 2008. The data from a total 18 flights (70 h flight time) from near the surface to 2100 m altitude were obtained with a Yun-12 aircraft in the southern surrounding areas of Beijing (38–40° N, 114–118° E). The objectives of these measurements were to characterize the regional variation of air pollution during and after the Olympics of 2008, determine the importance of air mass trajectories and to evaluate of other factors that influence the pollution characteristics. The results suggest that there are primarily four distinct sources that influenced the magnitude and properties of the pollutants in the measured region based on back-trajectory analysis: (1) southerly transport of air masses from regions with high pollutant emissions, (2) northerly and northeasterly transport of less pollutant air from further away, (3) easterly transport from maritime sources where emissions of gaseous pollutant are less than from the south but still high in particle concentrations, and (4) the transport of air that is a mixture from different regions; that is, the air at all altitudes measured by the aircraft was not all from the same sources. The relatively long-lived CO concentration is shown to be a possible transport tracer of long-range transport from the northwesterly direction, especially at the higher altitudes. Three factors that influenced the size distribution of particles – i.e., air mass transport direction, ground source emissions and meteorological influences – are also discussed.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference44 articles.
1. Agarwal, J. K. and Sem, G. J.: Continuous flow, single-particle-counting condensation nucleus counter, J. Aerosol Sci., 11, 343–357, 1980. 2. Beijing Organizing Committee for the Games of the XXIX Olympic Games (BOCOG): Green Olympics in Beijing 2005, available at: http://en.beijing2008.cn/30/79/article212027930.shtml (last access: 5 January 2014), 2005. 3. Dickerson, R. R., Li, C., Li, Z., Marufu, L. T., Stehr, J. W., McClure, B., Krotkov, N., Chen, H., Wang, P., Xia, X., Ban, X., Gong, F., Yuan, J., and Yang, J.: Aircraft observations of dust and pollutants over northeast China: Insight into the meteorological mechanisms of transport, J. Geophys. Res., 112, D24S90, https://doi.org/10.1029/2007JD008999, 2007. 4. Draxler, R. R. and Rolph, G. D.: HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory), Model access via NOAA ARL READY Website, http://www.arl.noaa.gov/HYSPLIT.php (last access: 5 January 2014), NOAA Air Resources Laboratory, College Park, MD, 2013. 5. Elperin, T., Fominykh, A., Krasovitov, B., and Vikhansky, A.: Effect of rain scavenging on altitudinal distribution of soluble gaseous pollutants in the atmosphere, Atmos. Environ., 45, 2427–-2433, 2011.
Cited by
21 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|