Atmos. Chem. Phys. Discuss., 11, 8337-8384, 2011
www.atmos-chem-phys-discuss.net/11/8337/2011/
doi:10.5194/acpd-11-8337-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
The fate of Saharan dust across the Atlantic and implications for a Central American dust barrier
E. Nowottnick1, P. Colarco2, A. da Silva3, D. Hlavka4, and M. McGill4
1Atmospheric and Oceanic Sciences, University of Maryland, College Park, MD, USA
2Code 613.3, NASA Goddard Space Flight Center, Greenbelt, MD, USA
3Code 610.1, NASA Goddard Space Flight Center, Greenbelt, MD, USA
4Code 613.1, NASA Goddard Space Flight Center, Greenbelt, MD, USA

Abstract. Saharan dust was observed over the Caribbean basin during the summer 2007 NASA Tropical Composition, Cloud, and Climate Coupling (TC4) field experiment. Airborne Cloud Physics Lidar (CPL) and satellite observations from MODIS suggest a barrier to dust transport across Central America into the eastern Pacific. We use the NASA GEOS-5 atmospheric transport model with online aerosol tracers to perform simulations of the TC4 time period in order to understand the nature of this barrier. Our simulations are driven by the Modern Era Retrospective-Analysis for Research and Applications (MERRA) meteorological analyses. We evaluate our baseline simulated dust distributions using MODIS and CALIOP satellite and ground-based AERONET sun photometer observations. GEOS-5 reproduces the observed location, magnitude, and timing of major dust events, but our baseline simulation does not develop as strong a barrier to dust transport across Central America as observations suggest. Analysis of the dust transport dynamics and lost processes suggest that while both mechanisms play a role in defining the dust transport barrier, loss processes by wet removal of dust are about twice as important as transport. Sensitivity analyses with our model showed that the dust barrier would not exist without convective scavenging over the Caribbean. The best agreement between our model and the observations was obtained when dust wet removal was parameterized to be more aggressive, treating the dust as we do hydrophilic aerosols.

Citation: Nowottnick, E., Colarco, P., da Silva, A., Hlavka, D., and McGill, M.: The fate of Saharan dust across the Atlantic and implications for a Central American dust barrier, Atmos. Chem. Phys. Discuss., 11, 8337-8384, doi:10.5194/acpd-11-8337-2011, 2011.
 
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