Atmos. Chem. Phys., 11, 1769-1790, 2011
www.atmos-chem-phys.net/11/1769/2011/
doi:10.5194/acp-11-1769-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
Characterizing summertime chemical boundary conditions for airmasses entering the US West Coast
G. G. Pfister1, D. D. Parrish2, H. Worden1, L. K. Emmons1, D. P. Edwards1, C. Wiedinmyer1, G. S. Diskin3, G. Huey4, S. J. Oltmans2, V. Thouret5,6, A. Weinheimer1, and A. Wisthaler7
1Atmospheric Chemistry Division, National Center for Atmospheric Research (NCAR), Boulder, CO, USA
2Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
3Chemistry and Dynamics Branch, NASA Langley Research Center, Hampton, VA, USA
4School of Earth & Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
5Laboratoire d'Aérologie, Centre National de la Recherche Scientifique, Toulouse, France
6Université de Toulouse, Toulouse, France
7Institute for Ion Physics & Applied Physics, University of Innsbruck, Innsbruck, Austria

Abstract. The objective of this study is to analyze the pollution inflow into California during summertime and how it impacts surface air quality through combined analysis of a suite of observations and global and regional models. The focus is on the transpacific pollution transport investigated by the NASA Arctic Research of the Composition of the Troposphere from Aircraft and Satellites (ARCTAS) mission in June 2008. Additional observations include satellite retrievals of carbon monoxide and ozone by the EOS Aura Tropospheric Emissions Spectrometer (TES), aircraft measurements from the MOZAIC program and ozonesondes. We compare chemical boundary conditions (BC) from the MOZART-4 global model, which are commonly used in regional simulations, with measured concentrations to quantify both the accuracy of the model results and the variability in pollution inflow. Both observations and model reflect a large variability in pollution inflow on temporal and spatial scales, but the global model captures only about half of the observed free tropospheric variability. Model tracer contributions show a large contribution from Asian emissions in the inflow. Recirculation of local US pollution can impact chemical BC, emphasizing the importance of consistency between the global model simulations used for BC and the regional model in terms of emissions, chemistry and transport. Aircraft measurements in the free troposphere over California show similar concentration ranges, variability and source contributions as free tropospheric air masses over ocean, but caution has to be taken that local pollution aloft is not misinterpreted as inflow. A flight route specifically designed to sample boundary conditions during ARCTAS-CARB showed a prevalence of plumes transported from Asia and thus may not be fully representative for average inflow conditions. Sensitivity simulations with a regional model with altered BCs show that the temporal variability in the pollution inflow does impact modeled surface concentrations in California. We suggest that time and space varying chemical boundary conditions from global models provide useful input to regional models, but likely still lead to an underestimate of peak surface concentrations and the variability associated with long-range pollution transport.

Citation: Pfister, G. G., Parrish, D. D., Worden, H., Emmons, L. K., Edwards, D. P., Wiedinmyer, C., Diskin, G. S., Huey, G., Oltmans, S. J., Thouret, V., Weinheimer, A., and Wisthaler, A.: Characterizing summertime chemical boundary conditions for airmasses entering the US West Coast, Atmos. Chem. Phys., 11, 1769-1790, doi:10.5194/acp-11-1769-2011, 2011.
 
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