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Detailed Reference Information |
Kulmala, M., Reissell, A., Sipilä, M., Bonn, B., Ruuskanen, T.M., Lehtinen, K.E.J., Kerminen, V. and Ström, J. (2006). Deep convective clouds as aerosol production engines: Role of insoluble organics. Journal of Geophysical Research 111: doi: 10.1029/2005JD006963. issn: 0148-0227. |
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Deep convection associated with thunderstorms and sometimes with frontal systems is an effective way to transport material from the planetary boundary layer to the upper troposphere and even to the lower stratosphere. Aerosol particles observed in clouds and in cloud outflows suggest that deep convection is an important source of particles in the upper troposphere. However, the detailed pathways by which the observed small particles could have been formed inside the clouds are unknown. In this paper we propose a hypothesis, where water insoluble trace gases that can survive the deep convective updraft are producing new particles at low temperatures near the tropopause. In order to be able to verify this new mechanism, laboratory experiments were designed to simulate this process. It was found that ambient water insoluble trace gases were indeed able to produce new aerosol particles by homogeneous nucleation under cloud like conditions. Therefore it seems that our hypothesis gives a plausible explanation for new particle production inside cloud anvils and cloud outflows. |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Atmospheric Composition and Structure, Aerosols and particles (0345, 4801, 4906), Atmospheric Composition and Structure, Cloud physics and chemistry, Atmospheric Composition and Structure, Exosphere, Atmospheric Composition and Structure, Pollution, urban and regional (0305, 0478, 4251) |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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