9. It seems 1.5°C has come down to semantics, "virtually impossible" versus "challenging"?
I see my job as a scientist to be frank on the challenges, but to doomsdayers, noting the challenges is not the same as giving up. Still plenty to fight for. cicero.oslo.no/no/posts/klima…
/end
Bonus tweet 1: I think the scientific community has done itself a disservice with framing carbon budgets as single numbers with a probability (eg 475 GtCO₂ for a 66% chance).
Better to use ranges (eg 760 GtCO₂ with 33–66% range 475–930 GtCO₂). rdcu.be/bHT2C
Bonus tweet 2: Using a single number gives a false precision, & leads to the "12 years to..." framing.
A range explicitly brings in the uncertainty, & allows more nuance to be given on the feasibility of 1.5°C. This would avoid much of this thread...
Bonus tweet 3: Here is the 5-95% temperature uncertainty for 1.5°C scenarios from two simple climate models (FAIR, MAGICC) used in SR15. The peak temperature ranges from 1.1°C to >2°C.
If FAIR is correct, 1.5°C is not 'virtually impossible'...
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'Net' emissions are a slippery slope, but we already deal with net emissions. It is not so scary...
In most Annex I countries LULUCF emissions are a net-sink. The sink is mainly forest regrowth & recovery.
Net emissions have been here since 1990, at least...
1/
In the EU, most of the sink is increased uptake in existing forests, there is a small part of afforestation (dark green). There are also emission sources, such as from grasslands & new settlements.
Maintaining the sink over time (with climate impacts) could be hard.
2/
The EU27 now includes the land sink (LULUCF) in its climate targets.
Perhaps this is good? It forces the EU to maintain & expand its sink.
Perhaps this is bad? The EU can now have 'net-zero' emissions in 2050 (though, studies suggest this is mainly agricultural)
Historically, the land & ocean sink have removed about one-half of the anthropogenic CO₂ emissions.
If we mitigate successfully in the future, the sinks will take up less CO₂ since emissions are lower, but they will be replaced by 'engineered sinks'.
1/n
This is a more detailed figure showing the anthropogenic CO₂ emission sources (top), & the land and ocean sinks (with the balance remaining in the atmosphere). Bread & butter carbon cycle...
IPCC: "In model pathways with no or limited overshoot of 1.5°C, global net anthropogenic CO₂ emissions [reach] net zero ~2050 (2045–2055)"
There are likely equally plausible scenarios (shown here) that reach net-zero CO₂ emissions in 2100 with the same 'carbon budget'.
1/
You don't believe me?
These are the scenarios used for net-zero ~2050 (2045-2055). They basically all cross zero around 2050. This is because they focus on 2100 targets & allow 'overshoot'.
This is a design feature of the scenarios, & are not the only way to get to 1.5°C!
2/
The temperature response to those scenarios all have a 'peak & decline' shape. Some of the 'peak & decline' is due to CO₂ emissions & some to non-CO₂ emissions (GWP100 confuses this point).
Most modelling uses a 2100 target, allowing overshoot (a cost-effective 'feature').
If we take a remaining carbon budget consistent with 1.5°C, then emissions need to drop rapidly. This curve converges to zero, there is no physical reason to have a straight line to zero.
(I took 580GtCO₂ from SR15 Table 2.2, not adjusted for time past)
IPCC AR5 WG3 (2014) had a figure showing the impact on mitigation costs of various technology restrictions (eg, no CCS).
It also compared lower energy demand (20–30% below baseline by 2050 & 35–45 % by 2100), first set of bars.
This 𝑟𝑒𝑑𝑢𝑐𝑒𝑑 mitigation costs by half.
1/
The 'low energy demand' analysis enforced a reduction on demand, but did not evaluate the costs (ie, mitigation costs of reduced demand are assumed zero).