We see far greater risk of massive irreversible sea level rise (SLR) at 2°C, on a scale of 12–20 meters or more in the long term. The climate record of the Earth over the pat few million years is quite clear:
Sea Level Rise from Ice Sheets
We see far greater risk of massive irreversible sea level rise (SLR) at 2°C, on a scale of 12–20 meters or more in the long term. The climate record of the Earth over the pat few million years is quite clear:
Sea Level Rise from Ice Sheets
What 1.5°C Pathways Look Like
The IPCC Special Report: Global Warming of 1.5°C made clear that
45-60% emissions reductions (median 50%) are needed by 2030
in order to reach carbon neutrality by 2050,
and remain close to 1.5°C of warming.
Global CO2 characteristics Pathways
limiting warming to 1.5°C
with no or limited overshoot
(less than 0.1°C):
Robust declining trend in next decade
Reach net-zero CO2 around mid-century
Varying levels of carbon-dioxide removal (CDR)
Non-CO2 emissions are also strongly reduced
but do not reach zero globally
Are these changes still feasible?
The IPCC found out that there are six tick boxes that need to be ticked if you want to be able to say that something is feasible.
✔️ Geophysical feasibility
✔️ Environmental feasibility
✔️ Technical feasibility
✔️ Economic feasibility
There are boxes that we scientists, can tick ourselves because we understand the physics, we understand how our Earth system works, we understand how technologies develop or we understand economics
But there are two dimensions where we scientists do not call the shots.
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Institutional feasibility: whether our political system can do this
Social and cultural feasibility: whether our societies are willing to change some of their behaviors that are currently resulting in very much pollution.
1.5° Consistent NDCs
Take a look at the countries following an emissions pathway compatible with a 1.5°C trajectory.
Overshoot NDCs
Take a look at the countries currently following an emissions pathway not compatible with a 1.5°C trajectory.
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Dr. Joeri Rogelj