The Amazon carbon sink is weakening as deforestation 1–5 , rising tree mortality 6–8 and climate change disrupt the climatic conditions that sustain a humid tropical forest 9–11 . Forest loss reduces precipitation, increases temperatures and lengthens the dry season, driving higher carbon emissions 1–4,11,12 . Climate stress is stronger in more deforested regions, rendering forests progressively more flammable 1,9,13 . Large-scale climate events, such as El Niño, further amplify regional climate impacts 9,14–17 . Here we present an analysis of 15 years of Amazonian carbon fluxes derived from atmospheric CO 2 measurements. We determine a carbon balance of 0.32 ± 0.08 PgC yr −1 , with fires acting as the dominant source (0.40 ± 0.07 PgC yr −1 ) and forest uptake becoming increasingly unable to offset emissions. Furthermore, we investigate key drivers of the carbon emissions of Amazonia and identify three distinct year groups. Group 1 (2011–2014, 2017 and 2018) represents the role of the Amazon in the global carbon balance (0.11 ± 0.08 PgC yr −1 ) during wetter years with low human activity, such as deforestation, biomass burning and degradation. Group 2 (2019–2022) represents Amazon carbon emissions (0.43 ± 0.13 PgC yr −1 ) from human activities (mainly deforestation and degradation) during years with low climatic stress. Group 3 (2010, 2015, 2016, 2023 and 2024) has the highest carbon emissions (0.49 ± 0.07 PgC yr −1 ) and comprises warm and dry years (high climate stress), such as El Niño and the warming of the Tropical North Atlantic Ocean, associated with biomass burning.
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Gatti et al. (2026) studied this question.
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