Abstract

Abstract. Simulated primary organic aerosols (POA), as well as other particulates and trace gases, in the vicinity of Mexico City are evaluated using measurements collected during the 2006 Megacity Initiative: Local and Global Research Observations (MILAGRO) field campaigns. Since the emission inventories, transport, and turbulent mixing will directly affect predictions of total organic matter and consequently total particulate matter, our objective is to assess the uncertainties in predicted POA before testing and evaluating the performance of secondary organic aerosol (SOA) treatments. Carbon monoxide (CO) is well simulated on most days both over the city and downwind, indicating that transport and mixing processes were usually consistent with the meteorological conditions observed during MILAGRO. Predicted and observed elemental carbon (EC) in the city was similar, but larger errors occurred at remote locations since the overall CO/EC emission ratios in the national emission inventory were lower than in the metropolitan emission inventory. Components of organic aerosols derived from Positive Matrix Factorization of data from several Aerodyne Aerosol Mass Spectrometer instruments deployed both at ground sites and on research aircraft are used to evaluate the model. Modeled POA was consistently lower than the measured organic matter at the ground sites, which is consistent with the expectation that SOA should be a large fraction of the total organic matter mass. A much better agreement was found when modeled POA was compared with the sum of "primary anthropogenic" and "biomass burning" components derived from Positive Matrix Factorization (PMF) on most days, especially at the surface sites, suggesting that the overall magnitude of primary organic particulates released was reasonable. However, simulated POA from anthropogenic sources was often lower than "primary anthropogenic" components derived from PMF, consistent with two recent reports that these emissions are underestimated. The modeled POA was greater than the total observed organic matter when the aircraft flew directly downwind of large fires, suggesting that biomass burning emission estimates from some large fires may be too high.

Highlights

  • Most predictions of organic matter made by threedimensional particulate models are currently significantly too low because the processes contributing to secondary organic aerosol (SOA) formation and transformation are not well understood

  • The Weather Research and Forecasting (WRF)-chem model is used with trace gas and particulate release rates derived from gridded versions of the 1999 National Emissions Inventory and the 2002 Mexico City Metropolitan Area (MCMA) as adjusted by Lei et al (2007) to predict primary organic aerosols (POA) and other tracers in the vicinity of Mexico City during the 2006 Megacity Initiative: Local and Global Research Observations (MILAGRO) field campaigns. Uncertainties in both the primary emission estimates and the simulated meteorological processes will affect predictions of total organic matter and total particulate matter; our objective is to assess the uncertainties in predicted POA before testing and evaluating the performance of SOA treatments

  • Even though a wide range of trace gases and particulates are included in the model, this study focuses on parameters useful to evaluate the simulated transport and mixing of POA over central Mexico

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Summary

Introduction

Most predictions of organic matter made by threedimensional particulate models are currently significantly too low because the processes contributing to secondary organic aerosol (SOA) formation and transformation are not well understood. One objective of the Megacity Initiative: Local and Global Research Observations (MILAGRO) field campaign (Molina et al, 2008) conducted during March 2006 was to obtain measurements of organic aerosols and precursors of secondary organic aerosols (SOA). The current under-prediction of organic aerosol mass will subsequently affect predictions of direct radiative forcing by affecting scattering and absorption of radiation in the atmosphere. Predictions of indirect radiative forcing will be affected as well because the size distribution and chemical composition will affect aerosol hygroscopic properties, activation of cloud condensation nuclei, ice nuclei, and cloud chemistry

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