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  In situ measurements of background aerosol and subvisible cirrus in the tropical tropopause region

Thomas, A., Borrmann, S., Kiemle, C., Cairo, F., Volk, M., Beuermann, J., Lepuchov, B., Santacesaria, V., Matthey, R., Rudakov, V., Yushkov, V., MacKenzie, A. R., & Stefanutti, L. (2002). In situ measurements of background aerosol and subvisible cirrus in the tropical tropopause region. Journal of Geophysical Research, 107(D24):. doi:10.1029/2001JD001385.

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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:
Thomas, A., 著者
Borrmann, S.1, 著者           
Kiemle, C., 著者
Cairo, F., 著者
Volk, M., 著者
Beuermann, J., 著者
Lepuchov, B., 著者
Santacesaria, V., 著者
Matthey, R., 著者
Rudakov, V., 著者
Yushkov, V., 著者
MacKenzie, A. R., 著者
Stefanutti, L., 著者
所属:
1Particle Chemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826291              

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キーワード: subvisual; cirrus; tropics; tropopause; background; aerosol
 要旨: [1] In situ aerosol measurements were performed in the Indian Ocean Intertropical Convergence Zone (ITCZ) region during the Airborne Polar Experiment-Third European Stratospheric Experiment on Ozone (APE-THESEO) field campaign based in Mahe, Seychelles between 24 February and 6 March 1999. These are measurements of particle size distributions with a laser optical particle counter of the Forward Scattering Spectrometer Probe (FSSP)-300 type operated on the Russian M-55 high- altitude research aircraft Geophysica in the tropical upper troposphere and lower stratosphere up to altitudes of 21 km. On 24 and 27 February 1999, ultrathin layers of cirrus clouds were penetrated by Geophysica directly beneath the tropical tropopause at 17 km pressure altitude and temperatures below 190 K. These layers also were concurrently observed by the Ozone Lidar Experiment (OLEX) lidar operating on the lower- flying German DLR Falcon research aircraft. The encountered ultrathin subvisual cloud layers can be characterized as (1) horizontally extending over several hundred kilometers, (2) persisting for at least 3 hours (but most likely much longer), and (3) having geometrical thicknesses of 100-400 m. These cloud layers belong to the geometrically and optically thinnest ever observed. In situ particle size distributions covering diameters between 0.4 and 23 mum obtained from these layers are juxtaposed with those obtained inside cloud veils around cumulonimbus (Cb) anvils and also with background aerosol measurements in the vicinity of the clouds. A significant number of particles with size diameters around 10 mum were detected inside these ultrathin subvisible cloud layers. The cloud particle size distribution closely resembles a background aerosol onto which a modal peak between 2 and 17 mum is superimposed. Measurements of particles with sizes above 23 mum could not be obtained since no suitable instrument was available on Geophysica. During the flight of 6 March 1999, upper tropospheric and lower stratospheric background aerosol was measured in the latitude band between 4degreesS and 19degreesS latitude. The resulting particle number densities along the 56th meridian exhibit very little latitudinal variation. The concentrations for particles with sizes above 0.5 m m encountered under these background conditions varied between 0.1 and 0.3 particles/cm(3) of air in altitudes between 17 and 21 km.

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言語: eng - English
 日付: 2002-12-19
 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: 18265
ISI: 000181253700008
DOI: 10.1029/2001JD001385
 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 (D24) 通巻号: 4763 開始・終了ページ: - 識別子(ISBN, ISSN, DOIなど): ISSN: 0747-7309