EGU26-8986, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-8986
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
PICO | Wednesday, 06 May, 11:01–11:03 (CEST)
 
PICO spot 5, PICO5.9
Long-Term High-Frequency Measurements of Atmospheric CO₂ and δ¹³CO₂ at Gosan: Implications for Source Characteristics in East Asia
Jihye Jang1, Jooil Kim3, Haklim Choi2, Jieun Choi2, Jaegeun Yun2, Jimin Jang2, Sumin Kim4, Daegeun Shin4, Sehwan Yang4, and Sunyoung Park1,2
Jihye Jang et al.
  • 1Department of Oceanography, Kyungpook National University,Daegu, Republic of Korea (lulurhdwn@gmail.com)
  • 2Kyungpook Institute of Oceanography, Kyungpook National University, Daegu, Republic of Korea
  • 3Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, USA
  • 4National Institute of Meteorological Sciences, Korea Meteorological Administration, Seogwipo, Republic of Korea

Atmospheric carbon dioxide (CO₂) and its stable carbon isotope composition (δ¹³C) provide important constraints on CO₂ sources and sinks; however, long-term high-frequency observations remain limited in East Asia.

This study presents continuous observations of atmospheric CO₂ and δ¹³CO₂ obtained at the Gosan station on Jeju Island, South Korea, from 2017 to 2025 using a cavity ring-down spectroscopy (CRDS) analyzer. The 9-year record is based on 1 Hz measurements aggregated into hourly mean values, with measurement precisions of 0.01 ppm for CO₂ and 0.05‰ for δ¹³CO₂.

The observations reveal pronounced seasonal cycles in both CO₂ and δ¹³CO₂, with mean seasonal amplitudes of approximately 8–10 ppm for CO₂ and 0.4–0.5 ‰ for δ¹³CO₂, exceeding those observed at global background sites and reflecting the continental–marine boundary characteristics of the Gosan station. From 2017 to 2021, both the CO₂ growth rate and the long-term decline in δ¹³CO₂ are broadly consistent with global background trends, whereas after 2022, notable deviations from global background behavior are observed in both CO₂ growth rates and δ¹³CO₂ trends. Superimposed on these background variations, pollution-influenced air masses exhibit pronounced changes in δ¹³CO₂. Yearly Keeling plot analysis of CO₂–δ¹³CO₂ relationships for pollution events indicates a progressive enrichment in isotopic source signatures over time, suggesting a temporal shift in dominant emission sources.

To investigate anthropogenic source characteristics associated with these pollution signals, high-CO₂ events are first classified based on air mass transport pathways, and further examined by incorporating high-frequency measurements of carbon monoxide (CO) and nitrous oxide (N₂O) provided by the National Institute of Meteorological Sciences (NIMS), which serve as complementary tracers of combustion-related and non-combustion emission influences, respectively.

How to cite: Jang, J., Kim, J., Choi, H., Choi, J., Yun, J., Jang, J., Kim, S., Shin, D., Yang, S., and Park, S.: Long-Term High-Frequency Measurements of Atmospheric CO₂ and δ¹³CO₂ at Gosan: Implications for Source Characteristics in East Asia, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-8986, https://doi.org/10.5194/egusphere-egu26-8986, 2026.