Abstract

Size resolved CCN activity and bulk chemical composition of atmospheric aerosols in the submicrometer size range were measured at Noto Ground-based Research Observatory (NOTOGRO), facing the Sea of Japan at the tip of Noto Peninsula, in autumn 2012. In the atmospheric measurement, the CCN efficiency spectra, where the CCN number fraction is plotted against the diameter of aerosols, were obtained for four different supersaturation (SS) conditions. The hygroscopicity parameter κ, which depends on the chemical composition of aerosols, was estimated from analysis of the CCN spectra. The CCN activation diameters of ambient aerosols were clearly larger than those of pure ammonium sulfate under all SS conditions. The bulk chemical composition derived by an aerosol chemical speciation monitor (ACSM) also indicated the significant mass fraction of organics in the submicrometer size range. The relationship between the estimated κ values and the CCN activation diameters suggests that organics contribute the aerosol mass especially in the size range of less than 100 nm. The contribution of organics observed in this study was more apparent than those of other sites in East Asia. The mass concentrations and chemical compositions of the aerosols varied with trajectory pathway, which caused large fluctuations in κ values especially at higher SS conditions. The negative correlations between organic mass fraction and the diameters of cloud droplet diameters were observed under low SS conditions (0.13% and 0.25%), suggesting that less-hygroscopic organics, that can suppress the initial growth rates of cloud droplets, were included during the periods of large organic mass concentrations.

Highlights

  • Atmospheric aerosols play an important role in controlling the Earth’s radiation balance and/or the hydrological system by acting as cloud condensation nuclei (CCN)

  • The slope of the CCN efficiency spectra of ambient aerosols around the dact were not as steep as those of (NH4)2SO4 aerosols. These results suggest that ambient aerosols observed at Noto Ground-based Research Observatory (NOTOGRO) were less CCN-active than pure (NH4)2SO4, and had heterogeneous chemical composition in the size range around dact

  • Simultaneous measurement of the size-resolved CCN activity and bulk chemical composition of the fine-mode aerosols were conducted at Noto Peninsula, Japan, which is located in the downwind region of the northeast part of the Asian Continent

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Summary

Introduction

Atmospheric aerosols play an important role in controlling the Earth’s radiation balance and/or the hydrological system by acting as cloud condensation nuclei (CCN). Simultaneous measurement of sizesegregated CCN activity and chemical composition of the ambient aerosols under controlled SS conditions is an effective method for better characterizing CCN activity of the ambient aerosols (e.g., Gunthe et al, 2009; Mochida et al, 2010; Rose et al, 2010). Some inorganic aerosols such as ammonium sulfate ((NH4)2SO4) are known as most effective and important CCN in the atmosphere (e.g., Pruppacher and Klett, 1997). It is important to know how the organics in the aerosols affect their CCN properties in the ambient atmosphere

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