Carbon budget for 1.5°C will run out in six years

If humanity wants to have a 50-50 chance of limiting global warming to 1.5°C, we can only emit 250 another gigatonnes (billion metric tonnes) of CO₂. This effectively gives the world just six years to get to net zero, according to calculations in new paper published in Nature Climate Change.

The global level of emissions is presently 40 gigatonnes of CO₂ per year. And, as this figure was calculated from the start of 2023, the time limit may be actually closer to five years.

Estimate is consistent with an assessment published by 50 leading climate scientists in June and updates with new climate data many of the key figures reported by the Intergovernmental Panel on Climate Change (IPCC) in August 2021.

How much CO₂ can still be emitted while remaining under a certain level of warming is referred to as the “carbon budget”. The carbon budget concept works because the increase in Earth’s global mean surface temperature has increased in a linear fashion with the total amount of CO₂ people have emitted since the industrial revolution.

The other side of this equation is that, roughly speaking, warming stops when CO₂ emissions stop: in other words, at net zero CO₂. This explains why net zero is such an important concept and why so many countries, cities, and companies have adopted net zero targets.

The study revised the remaining carbon budget down from the 500 gigatonnes reported by the the IPCC from the start of 2020. Some of this revision is merely timing: three years and 120 gigatonnes of CO₂ emissions later, the world is closer to the 1.5°C threshold. Improvements we made to the method for calculating budget adjustments shrank the remaining budget further.

Alongside CO₂, humanity emits other greenhouse gases and air pollutants that contribute to climate change. We adjusted the budget to account for the projected warming caused by these non-CO₂ pollutants. To do this, we used a large database of future emissions scenarios to determine how non-CO₂ warming is related to total warming.

Some of the warming caused by greenhouse gases is offset by cooling aerosols such as sulphates – air pollutants that are emitted along with CO₂ from car exhausts and furnaces. Almost all emissions scenarios project a reduction in aerosol emissions in the future, regardless of whether fossil fuels are phased out or CO₂ emissions continue unabated. Even in scenarios where CO₂ emissions increase, scientists expect stricter air quality legislation and cleaner combustion.

In its most recent report, the IPCC updated its best estimate of how much air pollution cools the climate. As a result, we expect that falling air pollution in future will contribute more to warming than previously assessed. This reduces the remaining 1.5°C budget by about another 110 gigatonnes.

Other updates made in the study to the carbon budget methodology tend to reduce the budget even more, such as projections of thawing permafrost that were not included in earlier estimates.

It is important to stress that many aspects of our carbon budget estimate are uncertain. The balance of non-CO₂ pollutants in future emissions scenarios can be as influential on the remaining carbon budget as different interpretations of how the climate is likely to respond.

We also do not know for sure whether the planet will really stop warming at net zero CO₂ emissions. On average, evidence from climate models tends to suggest it will, but some models show substantial warming continuing for decades after net zero is reached. If further warming after net zero is the case, the budget would be further reduced.

The risks of triggering tipping points such as the dieback of the Amazon rainforest increase – sometimes sharply – with increasing warming, but 1.5°C itself is not a hard boundary beyond which climate chaos abounds.