Record El Niño projected to push global temperatures to 1.91°C above pre-industrial levels
A record-breaking 2026-2027 El Niño is projected to temporarily raise global temperatures to 1.91°C, with the event contributing roughly one-fifth of the peak warming while anthropogenic warming drives most of the rise.
Why it matters
This forecast helps separate how much of the exceptional 2026-2027 warming is due to a natural climate event versus the underlying human-caused trend, which is important for interpreting temperature records and understanding extreme years. It shows that even an unprecedented El Niño occurs on top of an already-elevated baseline from greenhouse warming, demonstrating how natural variability and anthropogenic forcing interact.
What they did
The authors developed TESR, a statistical regression model that relates the El Niño-Southern Oscillation to global mean surface temperatures using monthly data from 1940 to July 2026. They validated the model through walk-forward testing against observations and compared it to a simple trend-ENSO baseline. They then used multi-model seasonal forecasts from August 2026 to project 2026-2027 global temperatures under a scenario of unprecedented El Niño intensity.
Key findings
- Central forecast is 1.91°C above pre-industrial levels in March 2027, with 100 percent probability of exceeding the 1.5°C Paris Agreement threshold from January 2027 onward
- Model attributes approximately 19 percent of the peak warming to the El Niño event, with anthropogenic background warming accounting for 84 percent of the total
- Probability of exceeding the 2.0°C threshold reaches 23-24 percent in March 2027; accounting for historical underestimation of peak temperatures suggests 45-60 percent probability
- Model achieves 47.4 percent reduction in forecast error compared to a simple trend-ENSO model, with a Brier Skill Score of 0.798 for probabilistic forecasts
Limitations
- The projected 2026-2027 ENSO amplitude exceeds the historical calibration range, making this an extrapolation beyond tested conditions
- The model assumes linear ENSO-temperature relationships even at extreme amplitudes where nonlinear saturation might occur
- Only the Niño 3.4 index is used as a predictor; other climate modes like the Pacific Decadal Oscillation and North Atlantic variability are not explicitly represented
Glossary
- GMSTA: Global Mean Surface Temperature Anomaly, the departure of global surface temperature from a reference period
- ENSO: El Niño-Southern Oscillation, a natural cycle of temperature variations in the tropical Pacific Ocean that affects global weather
- Niño 3.4 index: A measure of sea surface temperature in a tropical Pacific region used to define ENSO phases and intensity
- Ridge regression: A statistical technique that uses regularization to reduce overfitting and improve prediction stability
Original paper
Quantifying the impact of a projected Record-Breaking 2026–2027 El Niño on Global Temperatures using a Statistical Model
EGUsphere · 7 September 2026
This paper is a preprint. It has not been peer reviewed, and its results may change.
AI-generated summary of the original article; changes were made. Check the original before relying on it.