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Particle Formation in the Upper Tropical Troposphere: A Source of Nuclei for the Stratospheric Aerosol

Brock, C. A., Hamill, P., Wilson, J. C., Jonsson, H. H., Chan, K. R.·1995·Science

Abstract

Atmospheric measurements and numerical calculations described here indicate that binary homogeneous nucleation of H 2 SO 4 -H 2 O particles occurs in the upper tropical troposphere. Particle concentrations decrease with increasing altitude above the tropical tropopause as a result of coagulation during the upward air transport produced by stratospheric circulations. During the extended periods of time that volcanic eruptions do not strongly influence stratospheric particle number concentrations, particles formed in the upper tropical troposphere provide nuclei upon which oxidized sulfur gases condense in the stratosphere. This particle source, coupled with aerosol microphysical properties and atmospheric transport, governs the number concentration of particles in the lower tropical and mid-latitude stratosphere.

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Metadata

Authors
Brock, C. A., Hamill, P., Wilson, J. C., Jonsson, H. H., & Chan, K. R.
Venue
Science
Published
1995-12-08
Volume
270
Issue
5242
Pages
1650-1653
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2009409696
Cited by
216
References
0
FWCI
6.48
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Particle Formation in the Upper Tropical Troposphere: A Source of Nuclei for the Stratospheric Aerosol. https://app.cochat.ai/papers/10.1126/science.270.5242.1650
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Brock, C. A., Hamill, P., Wilson, J. C., Jonsson, H. H., & Chan, K. R. (1995). Particle Formation in the Upper Tropical Troposphere: A Source of Nuclei for the Stratospheric Aerosol. Science. https://doi.org/10.1126/science.270.5242.1650

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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