- 1Department of Earth System Science, Tsinghua University, Beijing, China (wanglx23@mails.tsinghua.edu.cn)
- 2Faculty of Information Technology, Monash University, Clayton, Australia
- 3Doerr School of Sustainability, Department of Earth System Science, Stanford University, Stanford, USA
Human heating- and cooling-induced CO2 emissions exhibit substantially different responses to extreme temperatures across countries, leading to satellite-detectable enhancements in atmospheric concentration. Quantifying this relationship is crucial for understanding human-climate interactions and informing targeted carbon mitigation policies. However, a global, systematic assessment has been hindered by the lack of timely, reliable, high-resolution carbon monitoring data. Satellite observations of the column-averaged dry-air mole fraction of CO2 (XCO2) always suffer from cloud-induced data gaps and overwhelming interference from natural fluxes, impeding anthropogenic signal extraction. Here, we integrate OCO-2/3 XCO2 and TROPOMI NO2 observations via machine learning to reconstruct global daily 0.1° XCO2 fields (2021-2023), and use local Moran’s I statistics to isolate anthropogenic XCO2 enhancements (XCO2en). The resulting XCO2en data exhibit distinct seasonal cycles across the world’s top-emitting regions, characterized by elevated levels in summer and winter. SHapley Additive exPlanations (SHAP) analysis reveals a consistent V-shaped relationship globally between temperature and its contribution to XCO2, indicating that both high and low temperature extremes elevate the SHAP value, with an optimal temperature (To) yielding the minimum value. Notably, despite vast differences in national temperature distributions, the To across countries converges around 21°C, suggesting a common human thermal adaptation threshold. Moreover, the slope of the V-shaped curve, representing the sensitivity of the XCO2en response to temperature, exhibits a significant positive correlation with national GDP per capita (R=0.50, p<0.01) and a negative correlation with the share of renewable energy consumption (R=-0.34, p<0.05). Our model effectively delineates the spatiotemporal patterns of anthropogenic XCO2en by leveraging carbon-nitrogen synergy, providing critical insights for decarbonization strategies and renewable energy transitions in diverse economies under carbon neutrality goals.
How to cite: Wang, L., Li, T., Song, X., Dou, X., Yu, Y., and Liu, Z.: Global anthropogenic XCO2 enhancements response to temperature changes with country-specific adaptability and sensitivity, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-10829, https://doi.org/10.5194/egusphere-egu26-10829, 2026.