Author/Authors :
Fujiwara، نويسنده , , Hiroshi and Sadanaga، نويسنده , , Yasuhiro and Urata، نويسنده , , Junki and Masui، نويسنده , , Yoshihiko and Bandow، نويسنده , , Hiroshi and Ikeda، نويسنده , , Keisuke and Hanaoka، نويسنده , , Sayuri and Watanabe، نويسنده , , Izumi and Arakaki، نويسنده , , Takemitsu and Kato، نويسنده , , Shungo and Kajii، نويسنده , , Yoshizumi and Zhang، نويسنده , , Daizhou and Hara، نويسنده , , Kazutaka and Fujimoto، نويسنده , , Toshiyuki and Seto، نويسنده , , Takafumi and Okuyama، نويسنده , , Kikuo and Ogi، نويسنده , , Takashi and Takami، نويسنده , , Akinori and Shimizu، نويسنده , , Atsushi and Hatakeyama، نويسنده , , Shiro، نويسنده ,
Abstract :
Aerial observations of atmospheric pollutants were made over the East China Sea to analyze the transport of air pollutants, especially nitrogen oxides, from East Asia. Three flights each were conducted in October 2009 (autumn) and December 2010 (winter). Onboard measurements of gaseous total odd nitrogen species, gaseous nitric acid (HNO3(g)), O3, SO2, CO and black carbon were made and particles were collected on filters for ionic and metal component analyses. The NO3−(p)/T.NO3 (T.NO3 = HNO3(g) + NO3−(p); NO3−(p) indicates particulate nitrate) ratios were less than 0.5 in most cases. Exceptions were 17 October and 11 December, when high concentrations of dust particles (Kosa) were transported. The average T.NO3/NOy (NOy indicates total odd nitrogen species) ratio in winter was 0.59, and that in autumn was 0.71. In addition, positive and negative correlations between NOy − T.NO3 and ozone were observed in autumn and winter, respectively. These results indicate that the main components of NOy − T.NO3 are NOx and its descendant photochemical products, such as peroxyacyl nitrates and alkyl nitrates, in winter and autumn, respectively. Ratios of Na+ to Cl− + NO3− in particles were close to the seawater ratio for observations in both autumn and winter, save for the Kosa events. The main NO3−(p) formation process was the reaction of HNO3(g) with sea salt aerosols during autumn and winter. On the other hand, NO3−(p) was generated by the reaction of HNO3(g) with dust particles and sea salt during the Kosa events. The fraction of NH4NO3 in NO3−(p) was very small.
Keywords :
Aerial observation , nitrate , Total odd nitrogen species , east asia