Tropical rainforests are among the most biodiverse and carbon-rich ecosystems on Earth — and among the most vulnerable to climate change. Long-standing concerns about "tipping points" — thresholds beyond which forests irreversibly shift to degraded states — have been difficult to quantify. This study, published in Earth System Dynamics, provides one of the first rigorous estimates of how tipping risk for tropical rainforests changes with different levels of global warming.
By combining hydroclimatic stress metrics with vegetation resilience indicators, we develop a framework that quantifies the probability of crossing critical thresholds across major tropical forest biomes — the Amazon, the Congo Basin, and Southeast Asian forests. The analysis reveals a deeply non-linear relationship: tipping risk does not simply scale with temperature increases, but accelerates sharply beyond 1.5–2°C of warming. At 3°C of warming, tipping risk is estimated to be several times higher than at 1.5°C — a multi-fold increase with profound implications for global climate targets.
The Amazon emerges as particularly sensitive, where the interaction between warming temperatures, reduced dry-season rainfall, and ongoing anthropogenic deforestation creates compounding pressures. Our results suggest that even a modest overshoot of the 1.5°C Paris Agreement target substantially raises the probability of large-scale forest dieback — transitions that, once triggered, may be impossible to reverse on human timescales.
Staying within 1.5°C is not merely an aspirational target — for tropical rainforests, it may be the difference between resilience and collapse. The non-linear nature of tipping risk means that every fraction of a degree of avoided warming carries disproportionately large ecological and climatic benefits.