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  STAAARTE-MED 1998 summer airborne measurements over the Aegean Sea: 1. Aerosol particles and trace gases

Formenti, P., Reiner, T., Sprung, D., Andreae, M. O., Wendisch, M., Wex, H., Kindred, D., Dewey, K., Kent, J., Tzortziou, M., Vasaras, A., & Zerefos, C. (2002). STAAARTE-MED 1998 summer airborne measurements over the Aegean Sea: 1. Aerosol particles and trace gases. Journal of Geophysical Research, 107(D21):. doi:10.1029/2001JD001337.

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資料種別: 学術論文
その他のタイトル : J. Geophys. Res.

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 作成者:
Formenti, P.1, 著者           
Reiner, T.1, 著者           
Sprung, D.2, 著者           
Andreae, M. O.1, 著者           
Wendisch, M., 著者
Wex, H., 著者
Kindred, D., 著者
Dewey, K., 著者
Kent, J., 著者
Tzortziou, M., 著者
Vasaras, A., 著者
Zerefos, C., 著者
所属:
1Biogeochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826286              
2Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826285              

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キーワード: aerosols; Aegean Sea; chemical composition; biomass burning; vertical profiles
 要旨: [1] We performed airborne measurements of sulfur dioxide (SO2), carbon monoxide (CO), and aerosol chemical/microphysical properties over the Aegean Sea. The data were collected on board the Met Office C-130 research aircraft in August 1998. High SO2 mixing ratios up to 18 ppb and aerosol sulfate levels up to 500 ppt were measured near Thessaloniki in northern Greece. The highest concentrations were observed at altitudes between 1 and 2 km, while near the surface much lower SO2 mixing ratios between 1 and 4 ppb were found. The pollution was transported southward over the Aegean Sea as far south as Crete, where SO2 mixing ratios up to 5 ppb were observed. The combined results of the SO2, aerosol sulfate, and particle size distribution measurements indicate air masses containing emissions with different ages, which range from a few hours to several days. Fossil fuel pollution observed over northern Greece is transported from eastern Europe (Bulgaria, Romania, and Turkey). Additionally, our measurements indicate significant contributions from forest fires, in particular from haze layers that originated ten days earlier from fires over the Northwestern Canadian territories, and had crossed the Atlantic and passed over Europe. CO layers 1 to 2 km deep were observed above 1 km. Often a double-layer structure with a secondary CO layer above 3.5 km was also observed. We estimate that the contribution of biomass burning to the CO measured over Greece is fourfold that of fossil fuel. The lower layer had a significant number of particles in the accumulation mode (N-p, size range 0.1-1 mum, ratio N-p/CO of the order of 2-6 cm(-3) (STP) ppb(-1)), while the upper layers were particle- depleted by convection and wet scavenging. The Aitken particle mode (size range 5-100 nm) was depleted both in the lower and in the upper layers. This suggests that the Aitken particles originally present in the lower layers had already grown to the accumulation mode size when detected.

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言語: eng - English
 日付: 2002-11
 出版の状態: 出版
 ページ: -
 出版情報: -
 目次: -
 査読: 査読あり
 識別子(DOI, ISBNなど): eDoc: 18174
ISI: 000180860300001
DOI: 10.1029/2001JD001337
 学位: -

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出版物 1

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出版物名: Journal of Geophysical Research
  出版物の別名 : J. Geophys. Res.
種別: 学術雑誌
 著者・編者:
所属:
出版社, 出版地: -
ページ: - 巻号: 107 (D21) 通巻号: 4450 開始・終了ページ: - 識別子(ISBN, ISSN, DOIなど): ISSN: 0747-7309