Increasingly negative tropical water-interannual CO<sub>2</sub> growth rate coupling.
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ABSTRACT: Terrestrial ecosystems have taken up about 32% of the total anthropogenic CO2 emissions in the past six decades1. Large uncertainties in terrestrial carbon-climate feedbacks, however, make it difficult to predict how the land carbon sink will respond to future climate change2. Interannual variations in the atmospheric CO2 growth rate (CGR) are dominated by land-atmosphere carbon fluxes in the tropics, providing an opportunity to explore land carbon-climate interactions3-6. It is thought that variations in CGR are largely controlled by temperature7-10 but there is also evidence for a tight coupling between water availability and CGR11. Here, we use a record of global atmospheric CO2, terrestrial water st
SUBMITTER: Liu L
PROVIDER: S-EPMC10284699 | biostudies-literature | 2023 Jun
REPOSITORIES: biostudies-literature
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