Measurement of Organic and Elemental Carbon in Fine Particulate Matter (PM2.5) in a Subalpine Region of Jirisan National Park, South Korea (2022~2024)
Organic carbon (OC) and elemental carbon (EC) in PM2.5 influence regional climate change by scattering and absorbing solar radiation. Recent attention has focused on the long-range transport of OC and EC to high-altitude regions due to their potential role in accelerating spring snowmelt. Although subalpine and alpine areas account for only about 1% of South Korea, these high-elevation zones are highly vulnerable to climate change and provide important insights into how ecosystems may respond and adapt in the future. We collected 29 PM2.5 samples near Nogodan Peak (1,440 m a.s.l.) in Jirisan National Park and 10 samples at Seoul National University (91 m a.s.l.) between March 2022 and April 2024 to quantify OC and EC concentrations. The mean concentrations and standard deviations of OC and EC were 2.0±1.4 and 0.2±0.1 μg m-3 in Jirisan, and 3.6±0.9 and 0.3±0.2 μg m-3 in Seoul, respectively. These concentrations are lower than previously reported values across ~20 sites in South Korea, likely due to the national reduction in PM2.5 during the study period. Given these lower concentrations, the effect of EC on snowmelt might have been small in Jirisan. High OC/EC ratios (Jirisan: 22.1; Seoul: 12.5) may reflect biomass burning or the formation of secondary organic aerosols. As biomass burning is projected to increase under future climate scenarios and may alter the source and composition of carbonaceous aerosols, long-term research is essential to better understand their potential impacts on high-altitude ecosystems.