EGU26-15734, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-15734
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 08 May, 11:25–11:35 (CEST)
 
Room M2
ΔXCO/ΔXCO2 characteristics over coal-fire areas in Xinjiang, China using a portable EM27/SUN FTIR spectrometer
Qiansi Tu1, Jiaxin Fang1, Frank Hase2, André Butz3, África Barreto4, Omaira García4, and Kai Qin5
Qiansi Tu et al.
  • 1School of Mechanical Engineering, Tongji University, Shanghai, China
  • 2Institute of Meteorology and Climate Research (IMK-ASF), Karlsruhe Institute of Technology (KIT), Eggenstein-Leopoldshafen, Germany
  • 3Institute of Environmental Physics, Heidelberg University, Heidelberg, Germany
  • 4Izaña Atmospheric Research Centre (IARC), Meteorological State Agency of Spain (AEMet), Tenerife, Spain
  • 5School of Environment and Spatial Informatics, China University of Mining and Technology, Xuzhou, China

Long-term coal spontaneous combustion (CSC) represents a severe and persistent threat, resulting in substantial waste of energy resources, significant environmental degradation, and serious risks to human health and safety. To better understand the emission characteristics of CSC, we conducted ground-based measurements of XCO₂, XCH₄, XCO and aerosol optical depth (AOD) using a Fourier-transform infrared spectrometer (EM27/SUN) within the COCCON network, in the Wugonggou coal-fire region near Fukang, Xinjiang.

Our results indicate that TROPOMI satellite data systematically underestimated XCO, with a mean bias of 4.53 ± 5.53 ppb (4.54%). For distinct enhancement events observed by COCCON, ΔXCO₂ and ΔXCO exhibit a strong correlation (R² = 0.6082), with a slope of 9.782 ppb/ppm (9.782 × 10⁻³ ppm/ppm). This value is lower than the CAMS inventory ratio of 13.52 × 10⁻³. This discrepancy arises primarily from their distinct spatial representativeness. The COCCON instrument, located within the coal fire region, captures intense local combustion emission. In contrast, the CAMS product represents a daily average over a much larger model grid cell, which dilutes strong local point sources like coal fires within a broader regional background. Additionally, correlation analysis shows that ΔXCO is more closely linked to AOD (R² = 0.2283) than either ΔXCO₂ or ΔXCH₄, underscoring the distinct behavior of CO in coal-fire plumes.

How to cite: Tu, Q., Fang, J., Hase, F., Butz, A., Barreto, Á., García, O., and Qin, K.: ΔXCO/ΔXCO2 characteristics over coal-fire areas in Xinjiang, China using a portable EM27/SUN FTIR spectrometer, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-15734, https://doi.org/10.5194/egusphere-egu26-15734, 2026.