No collapswashing

La climatologue suisse Sonia Seneviratne remarque, dans un entretien au « Monde », une forme de banalisation face aux événements extrêmes. Elle redoute le franchissement de points de bascule aux conséquences imprévisibles.

Les deux climatologues estiment, dans une tribune au « Monde », que nous sommes encore très loin du « plan d’action solide » annoncé par le président de la Conférence des parties pour maintenir « à portée de main » l’objectif de l’accord de Paris.

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 storage and precipitation data to investigate changes in the interannual relationship between tropical land climate conditions and CGR under a changing climate. We find that the interannual relationship between tropical water availability and CGR became increasingly negative during 1989–2018 compared to 1960–1989