Abstract

Carbonaceous species (organic carbon [OC] and elemental carbon [EC]) and inorganic ions of particulate matter less than 2.5 μm (PM2.5) were measured to investigate the chemical characteristics of long-range-transported (LTP) PM2.5 at Gosan, Jeju Island, in Korea in the spring and fall of 2008–2012 (excluding 2010). On average, the non-sea-salt (nss) sulfate (4.2 µg/m3) was the most dominant species in the spring, followed by OC (2.6 µg/m3), nitrate (2.1 µg/m3), ammonium (1.7 µg/m3), and EC (0.6 µg/m3). In the fall, the nss-sulfate (4.7 µg/m3) was also the most dominant species, followed by OC (4.0 µg/m3), ammonium (1.7 µg/m3), nitrate (1.1 µg/m3), and EC (0.7 µg/m3). Both sulfate and OC were higher in the fall than in the spring, possibly due to more common northwest air masses (i.e., coming from China and Korea polluted areas) and more frequent biomass burnings in the fall. There was no clear difference in the EC between the spring and fall. The correlation between OC and EC was not strong; thus, the OC measured at Gosan was likely transported across a long distance and was not necessarily produced in a manner similar to the EC. Distinct types of LTP events (i.e., sulfate-dominant LTP versus OC-dominant LTP) were observed. In the sulfate-dominant LTP events, air masses directly arrived at Gosan without passing over the Korean Peninsula from the industrial area of China within 48 hr. During these events, the aerosol optical depth (AOD) increased to 1.63. Ionic balance data suggest that the long-range transported aerosols are acidic. In the OC-dominant LTP event, a higher residence time of air masses in Korea was observed (the air masses departing from the mainland of China arrived at the sampling site after passing Korea within 60–80 hr).Implications: In Northeast Asia, various natural and anthropogenic sources contribute to the complex chemical components and affect local/regional air quality and climate change. Chemical characteristics of long-range-transported (LTP) PM2.5 were investigated during spring and fall of 2008, 2009, 2011, and 2012. Based on air mass types, sulfate-dominant LTP and OC-dominant LTP were observed. A long-term variation and chemical characteristics of PM2.5 along with air mass and satellite data are required to better understand long-range-transported aerosols.

Highlights

  • IntroductionAtmospheric aerosols play an important role in climate change by affecting the radiation balances both directly (light scattering and/or light absorbing) and indirectly (acting as cloud condensation nuclei [CCN], which affects the number concentration of cloud droplets and the lifetime of a cloud) (Solomon, 2007)

  • Atmospheric aerosols play an important role in climate change by affecting the radiation balances both directly and indirectly (Solomon, 2007)

  • Implications: In Northeast Asia, various natural and anthropogenic sources contribute to the complex chemical components and affect local/regional air quality and climate change

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Summary

Introduction

Atmospheric aerosols play an important role in climate change by affecting the radiation balances both directly (light scattering and/or light absorbing) and indirectly (acting as cloud condensation nuclei [CCN], which affects the number concentration of cloud droplets and the lifetime of a cloud) (Solomon, 2007). Aerosols affect human health, impair visibility, and impact heterogeneous reactions in the ambient atmosphere (Seinfeld and Pandis, 2012). These aerosols are either directly emitted into the ambient atmosphere from various sources (primary aerosols) or are produced by gas-to-particle conversion processes (secondary aerosols). In northeast Asia, various natural and anthropogenic sources, such as urban/industry, dust, biomass burning, and marine sources, contribute to the complex chemical components and mixing state of aerosols and affect local/regional air quality and climate change (Huebert et al, 2003; Seinfeld et al, 2004; Zhang and Iwasaka, 2004). It has been difficult to characterize long-range-transported fine particles solely by isolating them from locally produced particles

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