COVID-19 induced reduction of fossil-fuel emissions in 2020 altered the seasonal cycle of atmospheric CO2 at high latitudes

• The impacts of fossil-fuel emissions on CO 2 seasonal cycle were investigated based on atmospheric-transport simulations. • The CO 2 seasonal cycle amplitude significantly increased in 2020 compared to 2018−2019 at high-latitude sites. • The fossil-fuel emission declines accounted for 0.43 ± 0.12 ppm of the increases in the CO 2 seasonal cycle amplitude at high-latitudes in 2020 The seasonal cycle of atmospheric CO 2 is commonly assumed to be dominated by terrestrial carbon uptake and minimally affected by fossil-fuel CO 2 emissions (FF). However, the magnitude and extent of the influence of FF on the CO 2 seasonal cycle remain elusive. In the first half of year 2020, the outbreak of the coronavirus disease 2019 led to large reductions in FF, providing a testbed for understanding the impact of FF on the CO 2 seasonal cycle. Here, we utilized CO 2 observations from the global surface network and conducted atmospheric transport simulations with daily FF data to assess the effects of FF reductions in 2020 on the CO 2 seasonal cycle. We first found widespread increases of 1.10 ± 0.67 ppm in the CO 2 seasonal cycle amplitude (SCA) at high-latitude sites in 2020 compared to 2018−2019, which were equal to 170 ± 11% of the inter-annual variability of detrended SCA over the previous 20 years. Further, we attribute FF reductions to 0.43 ± 0.12 ppm of the observed SCA increases at high-latitude sites in 2020. At the Barrow site, FF reductions account for 31.9% of the SCA increase in 2020. The critical impact of FF on SCA increase does not suggest a larger decline in FF at high latitudes than mid-latitudes. Rather, the FF contributes more to SCA anomalies in magnitude at mid-latitudes than high latitudes. The localized impacts of anomalies in land-atmosphere carbon exchange fluxes generally exceeded the FF impacts on SCA anomalies at mid-latitudes, inducing varying changes in SCA across different mid-latitude sites. Our study thus presents a framework that may be extended further, where the knowledge of FF for the year 2020 versus other years, enables refinement of how atmospheric CO 2 concentration vary seasonally.

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Journal
Agricultural and Forest Meteorology
Published
2026-02-17
DOI
https://doi.org/10.1016/j.agrformet.2026.111071
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
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article

COVID-19 induced reduction of fossil-fuel emissions in 2020 altered the seasonal cycle of atmospheric CO2 at high latitudes

Yanchen Gui, Qiang Zhang, Josep Peñuelas, Philippe Ciais et al.
Agricultural and Forest Meteorology
Atmospheric and Environmental Gas Dynamics
article

COVID-19 induced reduction of fossil-fuel emissions in 2020 altered the seasonal cycle of atmospheric CO2 at high latitudes

Yanchen Gui, Qiang Zhang, Josep Peñuelas, Philippe Ciais, Shilong Piao, Zhe Jin, Kai Wang
article en

Abstract

• The impacts of fossil-fuel emissions on CO 2 seasonal cycle were investigated based on atmospheric-transport simulations. • The CO 2 seasonal cycle amplitude significantly increased in 2020 compared to 2018−2019 at high-latitude sites. • The fossil-fuel emission declines accounted for 0.43 ± 0.12 ppm of the increases in the CO 2 seasonal cycle amplitude at high-latitudes in 2020 The seasonal cycle of atmospheric CO 2 is commonly assumed to be dominated by terrestrial carbon uptake and minimally affected by fossil-fuel CO 2 emissions (FF). However, the magnitude and extent of the influence of FF on the CO 2 seasonal cycle remain elusive. In the first half of year 2020, the outbreak of the coronavirus disease 2019 led to large reductions in FF, providing a testbed for understanding the impact of FF on the CO 2 seasonal cycle. Here, we utilized CO 2 observations from the global surface network and conducted atmospheric transport simulations with daily FF data to assess the effects of FF reductions in 2020 on the CO 2 seasonal cycle. We first found widespread increases of 1.10 ± 0.67 ppm in the CO 2 seasonal cycle amplitude (SCA) at high-latitude sites in 2020 compared to 2018−2019, which were equal to 170 ± 11% of the inter-annual variability of detrended SCA over the previous 20 years. Further, we attribute FF reductions to 0.43 ± 0.12 ppm of the observed SCA increases at high-latitude sites in 2020. At the Barrow site, FF reductions account for 31.9% of the SCA increase in 2020. The critical impact of FF on SCA increase does not suggest a larger decline in FF at high latitudes than mid-latitudes. Rather, the FF contributes more to SCA anomalies in magnitude at mid-latitudes than high latitudes. The localized impacts of anomalies in land-atmosphere carbon exchange fluxes generally exceeded the FF impacts on SCA anomalies at mid-latitudes, inducing varying changes in SCA across different mid-latitude sites. Our study thus presents a framework that may be extended further, where the knowledge of FF for the year 2020 versus other years, enables refinement of how atmospheric CO 2 concentration vary seasonally.

Agricultural and Forest MeteorologyVol. 380
Consejo Superior de Investigaciones Científicas (ES), Peking University (CN), UK Centre for Ecology & Hydrology (GB), Laboratoire des Sciences du Climat et de l'Environnement (FR), Centre for Research on Ecology and Forestry Applications (ES), Tsinghua University (CN)
Openalex Percentile: Top 66%
Atmospheric and Environmental Gas Dynamics
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