全球“贡嘎”CO2反演系统构建及其在陆地碳循环领域的应用
ID:568 View Protection:ATTENDEE Updated Time:2026-04-02 11:41:57 Hits:116 Oral Presentation

Start Time:2026-04-27 09:00(Asia/Shanghai)

Duration:10min

Session:S3-11 专题3.11 气候环境与数学 » F21专题3.11 气候环境与数学

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Abstract
Accurate assessment of the size and distribution of carbon dioxide (CO2) sources and sinks is important for efforts to understand the carbon cycle and support policy decisions regarding climate mitigation actions. Satellite retrievals of the column-averaged dry-air mole fractions of CO2 (XCO2) have been widely used to infer spatial and temporal variations in carbon fluxes through atmospheric inversion techniques. In this study, we present a global spatially resolved terrestrial and ocean carbon flux dataset for 2015–2022. The dataset was generated by the Global ObservatioN-based system for monitoring Greenhouse GAses (GONGGA) atmospheric inversion system through the assimilation of Orbiting Carbon Observatory-2 (OCO-2) XCO2 retrievals. We describe the carbon budget, interannual variability, and seasonal cycle for the global scale and a set of TransCom regions. The 8-year mean net biosphere exchange and ocean carbon fluxes were -2.22 ± 0.75 and -2.32 ± 0.18 Pg C yr-1, absorbing approximately 23 % and 24 % of contemporary fossil fuel CO2 emissions, respectively. The annual mean global atmospheric CO2 growth rate was 5.17 ± 0.68 Pg C yr-1, which is consistent with the National Oceanic and Atmospheric Administration (NOAA) measurement (5.24 ± 0.59 Pg C yr-1). Europe has the largest terrestrial sink among the 11 TransCom land regions, followed by Boreal Asia and Temperate Asia. The dataset was evaluated by comparing posterior CO2 simulations with Total Carbon Column Observing Network (TCCON) retrievals as well as Observation Package (ObsPack) surface flask observations and aircraft observations. Compared with CO2 simulations using the unoptimized fluxes, the bias and root mean square error (RMSE) in posterior CO2 simulations were largely reduced across the full range of locations, confirming that the GONGGA system improves the estimates of spatial and temporal variations in carbon fluxes by assimilating OCO-2 XCO2 data. This dataset will improve the broader understanding of global carbon cycle dynamics and their response to climate change. The dataset can be accessed at https://doi.org/10.5281/zenodo.8368846.
Keywords
CO2反演
Speaker
金哲
博士后 北京大学

Submission Author
金哲 北京大学
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Important Date
  • Conference Date

    Apr 25

    2026

    to

    Apr 29

    2026

  • Apr 07 2026

    Draft paper submission deadline

  • Jun 17 2026

    Registration deadline

Sponsored By
未来大气科学论坛理事会
Organized By
河海大学海洋学院
南京大学南京赫尔辛基大气与地球系统科学学院
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