Airborne aerosol measurements in the tropopause region and the dependence of new particle formation on preexisting particle number concentration

Journal of Geophysical Research Atmospheres

Volumn 103, Issue D23, 1998, Pages 31255-31263

  De Reus, Marian ^a   Ström, Johan ^a   Kulmala, Markku ^b   Pirjola, Liisa ^b   Lelieveld, Jos ^b,c   Schiller, Cornelius ^c,d   Zöger, Martin ^c,d  

^a STOCKHOLM UNIVERSITY   (Sweden)

^b UNIVERSITY OF HELSINKI   (Finland)

^c UTRECHT UNIVERSITY   (Netherlands)

^d FORSCHUNGSZENTRUM JÜLICH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

AEROSOL FORMATION; AIRBORNE SURVEY; TROPOPAUSE;

EID: 0032553896     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/1998JD100011     Document Type: Article

References (5)

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2. Ayers, G. P., R. W. Gillett, and J. L. Gras, On the vapor pressure of sulphuric acid, Geophys. Res. Lett., 7, 433-436, 1980.
3. Bigg, E. K., A mechanism for the formation of new particles in the atmosphere, Atmos. Res., 43, 129-137, 1997.
4. Brasseur, G., and C. Granier, Mount Pinatubo aerosols, chlorofluorocarbons and ozone depletion, Science, 257, 1239-1242, 1992.
5. Zöger, M., et al., FISH: A new family of balloon-borne and airborne Lyman-α photofragment fluorescence hygrometers, J. Geophys. Res., in press, 1998.