Why Forests Stopped Absorbing Excess Carbon Dioxide ✛

Original: "Low latency global carbon budget reveals a continuous decline of the land carbon sink during the 2023/24 El Nino event"
arXiv:2504.09189 · 2025-04-12 · CC BY 4.0 · 1 min
In 2023, atmospheric carbon dioxide rose faster than in any year in the past 45 years. The culprit was not emissions but drought in tropical forests.

Every year, forests and soils absorb some of the carbon dioxide emitted by factories and cars. It is like the planet taking a breath. But in 2023, that breath was weak. Atmospheric carbon dioxide grew at a rate of 3.66 parts per million per year, faster than in any year in the past 45 years of measurements.

The culprit was the warm El Niño current in the Pacific Ocean. It alters weather worldwide and brings drought to tropical forests. When trees lack water, they close the pores on their leaves to avoid drying out. With water, carbon dioxide uptake also stops. The forest stops growing and absorbing carbon, while the soil continues to breathe it back out.

The Amazon suffered the most: it lost half of its capacity to absorb carbon dioxide. Drought affected 68% of the region.

Previously, such disruptions were only noticed a year later, when full reports came out. Now scientists have combined computer models of forests, rapid calculations for the ocean, and satellite measurements of carbon dioxide. It is like a pulse oximeter on a finger: the planet's breathing is visible almost immediately. The ocean tried to help and absorbed a bit more, but that only covered a small fraction of what the land failed to take up.

The 2023 Amazon drought was so severe that river levels fell to historic lows, and in some areas navigation completely ceased. The area affected by water deficit reached 68.2% of the region, more than in any previous El Niño since 1997.

A scenario in which tropical forests turn from a carbon sink into a source is explored in Kim Stanley Robinson's novel 'The Ministry for the Future', where a heat wave in India triggers a cascade of climate disasters. This work shows that such a transition is already occurring in reality during strong El Niño events.

Scientists
Fred HoyleMargaret BurbidgeWilliam Lawrence Bragg
Concepts
El Niño land carbon sink La Niña ENSO spring predictability barrier Oceanic Niño index relative ONI Warm water volume interannual variability recharge oscillator model Indian Ocean capacitor effect Jin-Timmermann model ERSST El Niño-Southern Oscillation Madden–Julian Oscillation