Investigation of regional variations in CO$_2$ growth rates : Integrating Emission Inventories and Atmospheric Observations

Yogesh Bali; Darja Cvetković; Juan Gancio; Adrián Gutiérrez-Arroyo; Sofia Vazquez Alferez; Xuan Tung Vu; Jin Yan; Pietro Zgaga; Fakhteh Ghanbarnejad; Nasrin Mostafavi Pak

arXiv · 2606.28462

Investigation of regional variations in CO$_2$ growth rates : Integrating Emission Inventories and Atmospheric Observations

Yogesh Bali·Darja Cvetković·Juan Gancio·Adrián Gutiérrez-Arroyo·Sofia Vazquez Alferez·Xuan Tung Vu·Jin Yan·Pietro Zgaga·Fakhteh Ghanbarnejad·Nasrin Mostafavi Pak

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Abstract

Atmospheric carbon dioxide (CO2) growth rates reflects the combined influence of anthropogenic emissions, biospheric carbon exchange, and climate variability. While climate mitigation is primarily evaluated using bottom-up emission inventories within political boundaries, there is a need to validate these emission reductions using atmospheric measurements. Here, we present a global top-down analysis of atmospheric CO2 growth rates using CAMS atmospheric CO2 reanalysis, EDGAR anthropogenic emissions, GOSIF dataset and the Southern Oscillation Index (SOI) as a measures of biospheric activity, to quantify the relative influence of human and natural drivers. We find that atmospheric CO2 growth rate varies substantially across space and time but is dominated by natural carbon-cycle processes and global background trends. Anthropogenic emission signals are frequently masked by natural variability, making regional top-down detection of human emission changes difficult. The COVID-19 emission reductions in 2020, despite occurring during a neutral ENSO year, were not consistently reflected in regional atmospheric CO2 growth rates, highlighting the dominant roles of biospheric dynamics and atmospheric transport. Using unsupervised clustering and persistence analysis, we identify five characteristic carbon-cycle regimes. Spatial averaging removes much of the regional variability, leaving large-scale climate as the dominant control in most regimes. The active biosphere is the main exception, where strong biogenic signals persist, underscoring the critical role of tropical forests in shaping atmospheric CO2 variability.

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Yogesh Bali, Darja Cvetković, Juan Gancio, Adrián Gutiérrez-Arroyo, Sofia Vazquez Alferez, Xuan Tung Vu, Jin Yan, Pietro Zgaga, Fakhteh Ghanbarnejad, Nasrin Mostafavi Pak. 2026-06-26. Investigation of regional variations in CO$_2$ growth rates : Integrating Emission Inventories and Atmospheric Observations. https://arxiv.org/abs/2606.28462

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