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Volume 9, issue 13
Atmos. Chem. Phys., 9, 4363-4385, 2009
https://doi.org/10.5194/acp-9-4363-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 9, 4363-4385, 2009
https://doi.org/10.5194/acp-9-4363-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  07 Jul 2009

07 Jul 2009

Aerosol composition of the tropical upper troposphere

K. D. Froyd1,2, D. M. Murphy1, T. J. Sanford1,2, D. S. Thomson1,2, J. C. Wilson3, L. Pfister4, and L. Lait5 K. D. Froyd et al.
  • 1NOAA Earth System Research Laboratory, Chemical Sciences Division, Boulder, CO, USA
  • 2Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, CO, USA
  • 3Department of Mechanical and Materials Engineering, University of Denver, Denver, CO, USA
  • 4NASA Ames Research Center, Moffett Field, CA, USA
  • 5Goddard Earth Sciences and Technology Center, University of Maryland Baltimore County, Baltimore, MD, USA

Abstract. Aerosol composition was measured by the NOAA single-particle mass spectrometer (PALMS) aboard the NASA WB-57 high altitude aircraft platform during two Aura Validation Experiment (AVE) campaigns based in Costa Rica in 2004 and 2006. These studies yielded the most complete set of aerosol composition measurements to date throughout the tropical tropopause layer (TTL) and tropical lower stratosphere. We describe the aerosol properties of the tropical atmosphere and use composition tracers to examine particle sources, the role of recent convection, and cirrus-forming potential in the TTL. Tropical dynamics and regional air sources played principal roles in dictating tropospheric aerosol properties. There was a sharp change in aerosol chemical composition at about 12 km altitude coincident with a change in convective influence. Below this level, maritime convection lofted condensable material that generated acidic, sulfate-rich aerosol. These particles contained significant amounts of methanesulfonic acid (MSA) and showed evidence of cloud processes. In contrast, continental convection injected particles and precursors directly into the TTL, yielding a population of neutralized, organic-rich aerosol. The organics were often highly oxidized and particles with oxidized organics also contained nitrate. Above the tropopause, chemical composition gradually changed toward sulfuric acid particles but neutralized particles were still abundant 2 km above the tropopause. Deep continental convection, though sporadic and geographically localized, may strongly influence TTL aerosol properties on a global scale. The abundance of organic-rich aerosol may inhibit ice nucleation and formation of tropopause level cirrus.

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