@timinmitcham@kmac@bataille_chris@SvenTeske@JoeriRogelj@IEA I have not put all the IEA WEO2019 into my system, but I show what I have. CO2 was tweeted earlier. I show a figure for 1.5C (no and low overshoot from IPCC) & Lower 2C (around 66% <2C). IEA is sort of in between in terms of carbon budget (I think).
Overall, I don't see much evidence that the IEA is pro-fossil in comparison to many other scenarios, & some other scenarios are far more pro fossil because of CCS.
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.
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 😍🥰😘
1/
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.
2/
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!
3/
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.
2/
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
1/
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.
2/
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).