The recent IPCC report had a big focus on methane (CH4) – and rightly so. We should work to cut methane emissions quickly, but not at the expense of cutting CO2.
Methane is temporary, while CO2 is forever.
A quick thread: 1/13
Methane is a strong greenhouse gas – over 100x more effective at trapping heat than CO2 while its in the atmosphere. Its responsible for around 28% of positive radiative forcing (and historical warming). 2/
However, methane has a short atmospheric lifetime. Most of the methane we emit this year will be gone from the atmosphere in around a decade. Methane interacts with hydroxyl radicals (OH) in the atmosphere, and ultimately breaks down into (mostly) CO2 and H2O. 3/
This has an important implication: the amount of methane in the atmosphere depends largely on our rate of emissions. To put it a different way, if we emit 1 ton of methane per year for a decade or so, the amount of methane in the atmosphere will increase by around 10 tons. 4/
If we keep emitting 1 ton of methane, the amount in the atmosphere will stay around 10 tons. If we stop emitting methane, the amount in the atmosphere will quickly decrease. Its determined by the rate of our emissions over a 10-year or so average (e.g. the lifetime of methane) 5/
CO2 is very different. While around 60% of our CO2 emissions is taken up by the oceans and biosphere, much of the remainder sticks around for tens of thousands of years. CO2 does not break down in the atmosphere; rather it accumulates. 6/
This means the amount of CO2 in the atmosphere is based not on the rate of our emissions – as is the case for methane – but rather on our cumulative emissions. The difference is quite clear when we compare what happens when we emit 1 ton of CO2 and 1 ton of methane each year: 7/
This has some very important implications for our climate. First, if we increase methane emissions we warm the planet. If we keep methane emissions flat the planet does not warm (much*).
*CH4 oxidizes into CO2, but the amount of total CO2 coming from CH4 is pretty minor. 8/
For CO2, on the other hand, if we keep emissions flat the planet continues to warm. If we reduce emissions the planet continues to warm. As long as CO2 emissions are (much) above zero, the planet continues to warm. 9/
Second, if we cut methane emissions the planet cools quickly, as atmospheric methane falls. If we cut CO2 emissions, the planet warms more slowly. We cannot really cool the planet by cutting CO2, unless we actively suck more CO2 out of the atmosphere than we are emitting. 10/
This makes methane a much more powerful lever to affect short term warming. It also means if we cut methane today or a decade from now the long-term climate effects are largely the same (provided we at least stop methane emissions from increasing). 11/
However, if we wait to cut CO2 – say, because we prioritize cutting methane today – we will be stuck with additional warming from CO2 accumulating in the atmosphere that is much harder to deal with in the future. 12/
We can both reduce methane and CO2 emissions in the near term. But we need to be careful in cases when there are tradeoffs. CO2 is ultimately the main climate villain; methane is just its sidekick. The longer we wait to cut CO2 emissions the more warming we will lock in. 13/
There's grim news in the IPCC report, but also reasons for hope. We're flattening the curve of future emissions, and the darkest climate futures a decade ago are much less likely now. We can both celebrate progress and acknowledge how far we have to go: thebreakthrough.org/issues/energy/… 1/
A decade ago the world seemed on track for a particularly grim climate future. China was building a new coal plant every three days; global emissions were increasing at a rate of 3% per year and increased by 31% between 2001 and 2010. 2/
Scenarios where global carbon emissions tripled by the end of the 21st century with coal use increasing sixfold seemed plausible to many. Researchers argued that “business as usual” would likely lead to a world 4ºC or 5ºC above pre-industrial levels by 2100. 3/
In my latest piece at @CarbonBrief, I take a deep dive into what the IPCC AR6 says about when the world will likely pass 1.5C and 2C, and how the new estimates of the remaining carbon budgets compare to those in the 2018 IPCC SR15 special report: carbonbrief.org/analysis-what-… 1/14
When we talk about passing a particular warming level like 1.5C or 2C we are not referring to an individual year (or month). Any given year may be ~0.2C warmer or cooler than average due to natural variability from El Nino and La Nina events. 2/
The AR6 reports on the 20-year period in which temps exceed 1.5C (e.g. 2021-2040), and suggests using the midpoint of that range (e.g. 2030) as the year when long-term average temps passes that level. We used a similar approach in an earlier analysis: carbonbrief.org/analysis-when-… 3/
The IPCC 6th Assessment Report features a new emissions scenario – SSP1-1.9 – limiting warming to 1.5C in 2100 with limited overshoot. It requires the world reach net-zero by 2055.
However, under the hood it assumes a huge amount of negative emissions over the 21st century. 1/5
The assessed "carbon budget" to limit warming to 1.5C in the IPCC report is around 500 GtCO2.
However, the SSP1-1.9 scenario emits 700 GtCO2 during the 21st century, blowing way past the remaining carbon budget. At the same time, it deploys 430 GtCO2 of negative emissions. 2/5
Relying on negative emissions allows the scenario to have a more plausible emissions reductions pathway; a similar scenario not using any net-negative emissions would likely require getting to global net-zero emissions in the 2040s. 3/5
The new IPCC 6th Assessment Report (AR6) provides an unprecedented degree of clarity about the future of our planet, and the need to reduce – and ultimately eliminate – our emissions of greenhouse gases.
In this thread I take a look at some key findings from the report: 1/27
Perhaps most importantly, this report gives us a much clearer view of our climate future.
It does this by narrowing the range of climate sensitivity – which had remained largely unchanged since 1979 at "likely" between 1.5C and 4.5C warming if atmospheric CO2 is doubled. 2/
The new AR6 report gives a "likely" (e.g. 67% chance) climate sensitivity range of 2.5C to 4C, a full 50% reduction in uncertainty relative to the likely range given in the AR5. The AR6 "very likely" (~90% chance) range is 2C to 5C, compared to 1C to 6C in the AR5. 3/
This really is a key and under-appreciated challenge of climate mitigation in the US. We have become functionally unable to build big projects on time and on budget, and our litigation-driven approach to regulatory enforcement regularly holds up projects for decades.
I don't think people quite realize the scale of stuff that needs to be built to fully decarbonizing our economy by 2050. We will double or triple electricity generation, replace almost all our energy production, and build massive amounts of new transmission.
It will be hard to accomplish this without substantial regulatory reform. While we should not run roughshod over communities – particularly historically disadvantaged ones – we also need mechanisms to keep reflexive NIMBYism from delaying decarbonization.
I really wish people would take time to understand the actual issue in question before tweeting hot takes. The @ScienceMagazine article is discussing high climate sensitivity of some models; it rather by definition has nothing to do with plausibility of future emissions scenarios
We covered the implausible sensitivity values in some CMIP6 models - and their disagreement with observations - last year. The solution, as the Science piece discusses, is to give more weight to models that better match observations. thebreakthrough.org/issues/energy/…
As we discussed in a review last year, there is actually strong evidence to narrow the range of climate sensitivity, both on the high end but especially on the low end: sciencemag.org/news/2020/07/a…