2. Contrary to the view of many, the Sustainable Development Scenario (SDS) was already quite aggressive (~1.65°C).
The Net-Zero 2050 Scenario (NZE2050) is more aggressive than the SDS on power & end-use, but also includes some additional behavioural measures.
3. The thing with the behavioural measures is that you have to do a lot of them, & they are quite specific & targeted. This is on top of aggressive technological change.
The point is that 1.5°C requires pulling on pretty much every level, to the max. Now, not tomorrow.
4. Coal use takes a dive in NZE2050, basically a 75% drop in the next decade. This will require massive coal closures, particularly in the developing world.
The Stated Policies Scenario (STEPS) sees coal declining. For coal, it is a matter of how fast it goes, not if it goes.
5. Oil has a more gradual reduction, basically, reductions are easier elsewhere (eg coal).
This is the same with the scenarios assessed by the IPCC (light blue), it is not as if the IEA is turning up oil & doing something different. Even the SDS is in the range of IPCC 1.5°C...
6. The oil "decline rate is still slower than the underlying rate of decline in supply ... means that some upstream investment in oil would still be needed even in the NZE2050 world of rapidly falling oil demand."
This will annoy some people, but this is the same with the IPCC!
7. The IPCC says much the same on oil (& gas), but in a less direct way.
I am perhaps labouring on this point, but in terms of key characteristics of 1.5°C-2°C, there is little separating IEA & IPCC. A critique on the IEA for oil, applies equally to the IPCC.
8. Because the IEA & IPCC say there is space for more investment in oil & gas, does not mean it is a free for all.
The fundamental point is that there is considerably less oil in a 1.5°C than in a 3°C pathway, so oil investments need to fundamentally change.
9. The IEA gets away with a little more gas than many other scenarios, though will within the ranges. More gas just means less coal & oil (for a given carbon budget). Likewise, less gas means more coal & oil.
Comes back the IPCC, the literature is inconclusive on scale of gas.
10. Solar plays a strong role in NZE2050, initially following the same path as SDS, but then accelerating faster from 2025.
A key point here is that it is a lot more solar than in STEPS, which means more policy & support is needed to get solar on a path consistent with 1.5-2°C.
11. Overall, global primary energy use declines in 1.5°C scenarios, though many scenarios show an increase from 2030 onwards. This U shape is due to offsetting effects: efficiency improvements & fuel switching are eventually offset by growing demand (but less than today).
12. One good thing about the IEA is the additional sector detail. Here, for example, is how the transport sector changes: by 2030, over 50% of passenger cars sold in the NZE2050 are electric.
This sort of detail is hard to find in other scenarios.
13. There is a lot of detail in the WEO chapter on net-zero. I have shown a few snippets, but there are 24 figures and a lot of discussion to give a good understanding what has to happen by 2030 for net-zero in 2050.
14. The chapter focuses on 2030, so there is little detail on what has to happen from 2030 to 2050, and how net-zero is maintained after 2050.
But, this is all moot unless the reductions happen by 2030, so the focus is completely justified.
15. I am a little curious how the IEA critiques respond to this. Will they continue to focus on critiquing IEA from different angles, or help the IEA elevate & focus on the importance of 1.5°C. The IEA gives a blow-by-blow description to 2030, only need to implement?
16/16. Another great report from the @IEA, & great work led by @Laura_Cozzi_ & @tgouldao. Not only was net-zero & 1.5°C elevated, but COVID-19 was fully integrated into the scenarios. All while under difficult working conditions. Impressive!
We have a new paper in @nature on nitrous oxide (N₂O), five years in the making!
Like many GHGs, N₂O concentrations have been stable for thousands of years, but that balance between sources & sinks has been dramatically changed by humans.
2. N₂O is a potent GHG, 300 times worse than CO₂ over 100 years (GWP). It destroys the ozone layer & contributes to water pollution.
N₂O is ~7% of current radiative forcing, but because of its long lifetime & difficulty to mitigate, this will increase even in 1.5°C scenarios.
3. N₂O comes almost equally from natural (60%) & anthropogenic sources (40%).
Natural sources are dominated by microbial processes that break down nitrogen-containing compounds in the soil & oceans. These sources have previously balanced with the atmospheric chemical sinks.
There is often an assumption that the more aggressive climate targets means more BECCS.
This is only weakly true, many 2°C scenarios use as much BECCS as 1.5°C scenarios, & even >2.5°C scenarios use BECCS at scale!
IAMs just love BECCS 😍🥰😘
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These are scenarios that go over 2°C. Yes, some scenarios use over 20GtCO₂/yr in 2100 (we currently emit 40GtCO₂/yr). These are not aggressive mitigation scenarios, these are >2°C, & where we could end up with only weak climate policies like we have today.
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It is not that 1.5°C or 2°C (or even 3°C) needs large-scale BECCS, this is just the cost-effective pathway that most IAMs find. This could be for a variety of structural reasons.
Since BECCS is so prolific in scenarios, we obsess over it. It may just be a model artifact!
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Even though N₂O’s Ozone Depletion Potential is only 0.017, roughly one-sixtieth of CFC-11s, the large anthropogenic N₂O emissions make N₂O the single most important source of ozone depletion (that was in 2009!)
For the emission metric nerds out there, there is a close historical link between the Global Warming Potential (GWP) and the Ozone Depletion Potential (ODP).
The paper uses GWP & ODP, to contrast climate & ozone impacts.
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If you want to understand the GWP, read up on the ODP...
In this paper on the integrated Global Temperature change Potential (iGTP) I dug into some of the history, & it made me understand the GWP much better...
The results of yesterdays poll on EU climate ambition.
There was some ambiguity with the question, essentially to what degree the EU should adjust to the ambition of others.
There was a reason for the way I posed the question, around net-zero, linking to the ">2°C" option
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Scenarios with 50% chance of staying below 2°C rarely reach net-zero GHG by the end of the century (from IPCC SR15). The EU is aiming for net-zero GHG in 2050. The EU, in this case, would be more than 50 years ahead of the global average.
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This is the temperature response from those scenarios, still below 2°C (median in 2100 is 1.8°C).
So, to pick the option that the EU is consistent with over 2°C (>2°C in the poll) is rather extreme, & I would say inconsistent with the science (sorry).
"We estimate that 30 years of natural forest regrowth across 349 Mha & 678 Mha could [lead to uptake of 5.9 to 8.9 GtCO₂/yr]". This includes some below ground carbon.
Plenty to unpack, but how does it compare to emission scenarios?