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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • aerosol equilibrium
  • dust
  • chemical transport model

Index Terms

  • Atmospheric Composition and Structure: Ion chemistry of the atmosphere
  • Atmospheric Composition and Structure: Troposphere—composition and chemistry
  • Atmospheric Composition and Structure: Troposphere—constituent transport and chemistry
  • Meteorology and Atmospheric Dynamics: Numerical modeling and data assimilation
Abstract
Cited By (17)
 

Abstract

Three-dimensional simulations of inorganic aerosol distributions in east Asia during spring 2001

Youhua Tang

Center for Global and Regional Environmental Research, University of Iowa, Iowa City, Iowa, USA

Gregory R. Carmichael

Center for Global and Regional Environmental Research, University of Iowa, Iowa City, Iowa, USA

John H. Seinfeld

Departments of Chemical Engineering and Environmental Science and Engineering, California Institute of Technology, Pasadena, California, USA

Donald Dabdub

Department of Mechanical and Aerospace Engineering, University of California, Irvine, California, USA

Rodney J. Weber

School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA

Barry Huebert

School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii, USA

Antony D. Clarke

School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii, USA

Sergio A. Guazzotti

Department of Chemistry and Biochemistry, University of California, San Diego, California, USA

David A. Sodeman

Department of Chemistry and Biochemistry, University of California, San Diego, California, USA

Kimberly A. Prather

Department of Chemistry and Biochemistry, University of California, San Diego, California, USA

Itsushi Uno

Research Institute for Applied Mechanics, Kyushu University, Fukuoka, Japan

Jung-Hun Woo

Center for Global and Regional Environmental Research, University of Iowa, Iowa City, Iowa, USA

James J. Yienger

Center for Global and Regional Environmental Research, University of Iowa, Iowa City, Iowa, USA

David G. Streets

Decision and Information Sciences Division, Argonne National Laboratory, Argonne, Illinois, USA

Patricia K. Quinn

Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA

James E. Johnson

Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA

Chul-Han Song

Department of Environmental Science and Engineering, Gwangju Institute of Science and Technology (GIST), Gwangju, South Korea

Vicki H. Grassian

Center for Global and Regional Environmental Research, University of Iowa, Iowa City, Iowa, USA

Adrian Sandu

Department of Computer Science, Virginia Polytechnic Institute and State University, Blacksburg, Virginia, USA

Robert W. Talbot

Department of Earth Sciences, University of New Hampshire, Durham, New Hampshire, USA

Jack E. Dibb

Department of Earth Sciences, University of New Hampshire, Durham, New Hampshire, USA

In this paper, aerosol composition and size distributions in east Asia are simulated using a comprehensive chemical transport model. Three-dimensional aerosol simulations for the TRACE-P and ACE-Asia periods are performed and used to help interpret actual observations. The regional chemical transport model, STEM-2K3, which includes the on-line gas-aerosol thermodynamic module SCAPE II, and explicitly considers chemical aging of dust, is used in the analysis. The model is found to represent many of the important observed features. The Asian outflow during March and April of 2001 is heavily polluted with high aerosol loadings. Under conditions of low dust loading, SO2 condensation and gas phase ammonia distribution determine the nitrate size and gas-aerosol distributions along air mass trajectories, a situation that is analyzed in detail for two TRACE-P flights. Dust is predicted to alter the partitioning of the semivolatile components between the gas and aerosol phases as well as the size distributions of the secondary aerosol constituents. Calcium in the dust affects the gas-aerosol equilibrium by shifting the equilibrium balance to an anion-limited status, which benefits the uptake of sulfate and nitrate, but reduces the amount of aerosol ammonium. Surface reactions on dust provide an additional mechanism to produce aerosol nitrate and sulfate. The size distribution of dust is shown to be a critical factor in determining the size distribution of secondary aerosols. As much of the dust mass is found in the supermicron mode (70–90%), appreciable amounts of sulfate and nitrate are found in the supermicron particles. For sulfate the observations and the analysis indicate that 10–30% of sulfate is in the supermicron fraction during dust events; in the case of nitrate, more than 80% is found in the supermicron fraction.

Received 1 October 2003; accepted 24 February 2004; published 25 August 2004.

Citation: Tang, Y., et al. (2004), Three-dimensional simulations of inorganic aerosol distributions in east Asia during spring 2001, J. Geophys. Res., 109, D19S23, doi:10.1029/2003JD004201.

Cited By

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