There is a lot of confusion about carbon budgets and how quickly emissions need to fall to zero to meet various warming targets. To cut through some of this morass, we can use some very simple emission pathways to explore what various targets would entail. 1/11
Much confusion is due to ambiguity of these targets, role of negative emissions, non-CO2 forcings, historical warming, etc. For example, "well-below" 2C target in the Paris Agreement is often interpreted to mean a 66% chance of avoiding >2C warming. carbonbrief.org/analysis-why-t… 2/11
On the other hand, the 1.5C aspirational target is sometimes defined as a 50% chance of limiting warming to 1.5C, and sometimes (as in the new SSP1-1.9 scenario) as a 66% chance of avoidance. 3/11
Virtually all scenarios use negative emissions to expand the allowable budget; in the SSP 1.5C scenarios negative emissions effectively increases the size of the 420 GtCO2 budget by between 90% and 380%, allowing positive emissions of between 800 and 1600 GtCO2 by 2100 4/11
But leaving aside negative emissions (and their moral hazards) for the moment, the carbon budgets in the IPCC SR15 report make it relatively simple to calculate when emissions would have to reach zero under different climate targets: 5/11
If we assume that emissions simply linearly decrease until they reach zero, and look at four different interpretations of climate targets (66% chance of < 1.5C, 50% of < 1.5C, 66% of < 2C, 50% of < 2C), we get the figure below: 6/11
To have a 66% chance of avoiding 1.5C warming, emissions would have to fall 66% by 2030 and reach zero by 2036. For a 50% chance of 1.5C its a 46% reduction by 2030 and zero by 2043. For 2C 66% (50%) its 21% (16%) reduction by 2030 and zero by 2071 (2085). 7/11
However, these climate model-based budgets do not account for some earth system feedbacks from melting permafrost and methane released from wetlands. The SR15 suggests that including these would reduce all the carbon budgets by around 100 GtCO2. Here is what that looks like: 8/11
In this case to achieve a 66% (50%) chance of avoiding 1.5C, emissions would have to fall 92% (57%) by 2030 and reach zero by 2031 (2039). For a 66% (50%) chance of avoiding 2C warming we'd have to reduce emissions 24% (18%) by 2030 and reach zero in 2066 (2082). 9/11
One big takeaway from these simplified emission pathways is that limiting warming to 1.5C in the absence of planetary-scale negative emissions would be extremely difficult, requiring full decarbonization of the global economy in the next two decades. 10/11
At the same time, the pathways for limiting warming to <2C are much more forgiving, avoiding the need to bet the future on somewhat magical thinking around negative emissions deployment. 11/11
• • •
Missing some Tweet in this thread? You can try to
force a refresh
Theres been a bit of confusion lately around how the climate system response to carbon dioxide removal. While there are complexities, under realistic assumptions a ton of removal is still equal and opposite in its effects to a ton of emissions.
A thread: 1/x
When we emit a ton of CO2 into the atmosphere, a bit more than half is reabsorbed by the ocean and the biosphere today (though this may change as a warming world weakens carbon sinks). Put simply, 2 tons of CO2 emissions -> 1 ton of atmospheric accumulation.
Carbon removal (CDR) is subject to the same effects; if I remove two tons of CO2 from the atmosphere, the net removal is only one ton due to carbon cycle responses. Otherwise removal would be twice as effective as mitigation, which is not the case.
The carbon cycle has been close to equilibrium through the Holocene; we know this because we measure atmospheric CO2 concentrations in ice cores. But in the past few centuries CO2 has increased by 50%, and is now at the highest level in millions of years due to human emissions.
Starting 250 years ago, we began putting lots of carbon that was buried underground for millions of years into the atmosphere. All in all we’ve emitted nearly 2 trillion tons of CO2 from fossil fuels, which is more than the total mass of the biosphere or all human structures:
About a trillion of that has accumulated in the atmosphere, increasing CO2 concentrations to levels last seen millions of years ago. The remainder was absorbed by the biosphere and oceans. We can measure these sinks, and it’s incontrovertible that they are indeed net carbon sinks
We just published our State of the Climate Q2 update over at @CarbonBrief:
⬆️ Now a ~95% chance 2024 will be the warmest year on record.
⬆️ 13 month streak of records set between June 2023 and June 2024.
⬆️ July 22nd 2024 was the warmest day on record (in absolute terms).
⬇️ July 2024 will very likely come in below July 2023, breaking the record streak.
⬇️ The rest of 2024 is likely to be cooler than 2023 as El Nino fades and La Nina potentially develops.
⬇️ Second lowest Antarctic sea ice on record.carbonbrief.org/state-of-the-c…
The past 13 months have each set a new record, with 2024 being quite a bit warmer than 2023 (at ~1.63C above preindustrial levels) in the ERA5 dataset:
However, the margin by which records are being set has shrunk; global temperatures were setting new records by a stunning 0.3C to 0.5C in the second half of 2023, but have been breaking the prior records (set in 2016, 2020, or 2023) by only 0.1C to 0.2C this year:
Global surface temperatures from @BerkeleyEarth are now out for June. It was the warmest June on record for land, oceans, and the globe as a whole by a sizable margin (~0.14C), and came in at 1.6C above preindustrial levels. berkeleyearth.org/june-2024-temp…
This was the 13th consecutive record setting month, and the 12th month in a row above 1.5C:
The exceptional nature of recent global temperatures really stands out when we look at a 12-month moving average:
Global temperatures were extremely hot in June 2024, at just over 1.5C, beating June 2023's previous record-setting temperatures by 0.14C and coming in around 0.4C warmer than 2016 (the last major El Nino event).
Now 2024 is very likely to beat 2023 as the warmest year on record
June 2024 was so warm that – in the absence of 2023's exceptional warmth – it would have beaten any past July as the warmest absolute monthly temperature experienced by the planet in the historical record:
This plot shows how June 2024 stacked up against all the prior Junes since 1940 in the ERA5 dataset:
We’ve long talked about the carbon budget, but given that the world is on track to pass the 1.5C target in the coming decade its time to start talking about the "carbon debt".
Carbon dioxide accumulates in the atmosphere where it lasts for an extremely long time. While about half of our emissions are removed by land and ocean carbon sinks over the first century, it takes on the order of 400,000 years for nature to fully remove a ton of CO2.
But it turns out that the warming from our CO2 emissions is also extremely long lived. Even if global CO2 emissions ceased and atmospheric CO2 concentrations began to decline, the warming from those emissions would remain for millennia: pnas.org/doi/full/10.10…