Abstract

Abstract. Aerosol microphysical processes are essential for the next generation of global and regional climate and air quality models to determine particle size distribution. The contribution of organic aerosols (OAs) to particle formation, mass, and number concentration is one of the major uncertainties in current models. A new global–regional nested aerosol model was developed to simulate detailed microphysical processes. The model combines an advanced particle microphysics (APM) module and a volatility basis set (VBS) OA module to calculate the kinetic condensation of low-volatility organic compounds and equilibrium partitioning of semi-volatile organic compounds in a 3-D framework using global–regional nested domain. In addition to the condensation of sulfuric acid, the equilibrium partitioning of nitrate and ammonium, and the coagulation process of particles, the microphysical processes of the OAs are realistically represented in our new model. The model uses high-resolution size bins to calculate the size distribution of new particles formed through nucleation and subsequent growth. The multi-scale nesting enables the model to perform high-resolution simulations of the particle formation processes in the urban atmosphere in the background of regional and global environments. By using the nested domains, the model reasonably reproduced the OA components obtained from the analysis of aerosol mass spectrometry measurements through positive matrix factorization and the particle number size distribution in the megacity of Beijing during a period of approximately a month. Anthropogenic organic species accounted for 67 % of the OAs of secondary particles formed by nucleation and subsequent growth, which is considerably larger than that of biogenic OAs. On the global scale, the model well predicted the particle number concentration in various environments. The microphysical module combined with the VBS simulated the universal distribution of organic components among the different aerosol populations. The model results strongly suggest the importance of anthropogenic organic species in aerosol particle formation and growth at polluted urban sites and over the whole globe.

Highlights

  • The increased concentrations of atmospheric aerosol particles caused by anthropogenic activities have become an important scientific issue due to their substantial climate forcing and health effects (Twomey, 1977; Albrecht, 1989; Charlson et al, 1992; Donaldson et al, 2002; Tsigaridis et al, 2006; IPCC, 2013) on global and regional scales

  • hydrocarbon-like OAs (HOAs) and oxygenated OAs (OOAs) components obtained through positive matrix factorization (PMF) analysis were compared with the simulation results assuming they are primary and secondary components of organic aerosols (OAs) (i.e., primary OAs (POAs) and SOAs), respectively

  • Similar to black carbon (BC), the temporal variation of POAs is mainly influenced by emissions, transport, and deposition; the disagreement between the simulated POA and the observed HOA can largely be attributed to the emissions

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Summary

Introduction

The increased concentrations of atmospheric aerosol particles caused by anthropogenic activities have become an important scientific issue due to their substantial climate forcing and health effects (Twomey, 1977; Albrecht, 1989; Charlson et al, 1992; Donaldson et al, 2002; Tsigaridis et al, 2006; IPCC, 2013) on global and regional scales. These effects depend on aerosol size, composition, and mixing state. It is crucial to gain deep insight into the life cycle of aerosol particles and quantify their sources in mass concentration and in their number concentration

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