One of the most important findings in the recent IPCC report is that we ultimately determine how much warming will occur.
There is likely no warming "in the pipeline" once emissions get to zero. Rather, CO2 concentrations fall and temperatures stabilize https://t.co/SQl5waLZtRcarbonbrief.org/explainer-will…
Why does this happen? As emissions fall, land and ocean carbon sinks start taking up more CO2 than we emit, as they work through a backlog of our past emissions. This causes atmospheric CO2 to fall and (all things being equal) would cause cooling. bg.copernicus.org/articles/17/29…
At the same time, the oceans are continuing to absorb heat trapped by greenhouse gases, and their slow warming reduces ocean heat uptake from the atmosphere and warms the surface. It turns out that these two factors largely cancel each other out over time:
Of course, there are some caveats. The zero emissions commitment has some uncertainty (+/- 0.3C) across models. Adding in non-CO2 GHGs complicates the picture. And most scenarios examined focus on limiting warming to ~2C at net zero; higher warming might trigger more feedbacks.
But the takeaway is this: the warming the world will experience this century depends on our emissions. Its not too late, large amounts of future warming are not inevitable, but if we don't start reducing emissions soon we will lock in dangerous warming for centuries to come.
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The internet has been afire with speculation about a "termination shock" from the recent regulations on sulphur in marine fuel accelerating warming.
In a new @CarbonBrief post @piersforster and turn to climate models to help assess the potential impacts. carbonbrief.org/analysis-how-l…
As a bit of background, sulfur emissions (primarily SO2) have a strong cooling effect on the climate, both through directly scatting incoming sunlight (direct effects) and enhancing cloud formation (indirect effects). SO2 masks about half a degree of global warming today:
Global SO2 emissions have been decreasing since around the year 2000, contributing to a potential acceleration of the rate of warming over the last decade or so. At the same time, the climate "forcing" from aerosols remains highly uncertain (see the grey range below):
There is something weird happening at the UNFCCC. They argue removing 100 tons of CO2 for a single year and then re-releasing it can effectively offset a ton of fossil CO2 emissions.
The IPCC report was quite clear that the amount of warming is a largely time-independent function of cumulative emissions, and maintaining long-term net-zero emissions is required to stabilize temperatures.
Unless a framework is in place to compensate for future re-releases, using temporary CO2 removal to neutralize long-lived fossil CO2 emissions will ultimately result in higher global temperatures compared to emissions reductions or highly durable removals. files.carbonplan.org/Verra-Ton-Year…
Global emissions are now more or less tracking RCP4.5; the is particularly true if we look at fossil CO2, which is the most important factor in long-term growth (as its responsible for 90%+ of future emissions in high-end scenarios).
As the recent IPCC report made clear, under current policies we expect a plateauing of emissions continuing into the future:
Fascinating and timely paper by @bach_lennart, @_david_ho_, and colleagues on how to deal with air sea gas exchange uncertainties when assessing the effectiveness of ocean-based CDR. Sounds pretty nerdy, but its actually really important!
There are lots of proposed approaches to ocean CDR, including ocean alkalinity enhancement, direct ocean removal of CO2, and macro-algae (kelp) sinking. None of these directly remove CO2 from the atmosphere, however, and we need to figure out how long that would take!
If you are using CDR for making neutralization or offsetting claims, you should only be able to claim those tons when the atmospheric drawdown of CO2 actually occurs, otherwise its not reversing the climate effect of your emissions.
I often criticize the use of biosphere carbon removal to make neutralization claims for fossil CO2 given the fundamental mismatch in atmospheric/biosphere residence times.
But if you are trying to neutralize methane emissions, there is a case to be made for temporary CO2 removal
This is because the residence time of biosphere carbon is actually not that dissimilar from the residence time of atmospheric CH4 before it oxidizes, so their resulting climate effects should in turn be similar (provided you account for their different forcing magnitudes):
In other words, neutralizing CH4 from beef production by planting trees actually makes sense. Neutralizing CO2 from burning coal by planting trees generally does not.
Without warming, we would expect fewer and fewer new record high temperatures over time. In a new post over at The Climate Brink, @AndrewDessler explores why we are actually seeing more and more new records set (hint: the world is in fact warming). theclimatebrink.substack.com/p/why-are-ther…
In the absence of warming we'd expect the odds of setting a new record to decrease by 1/n over time, where n is the length of the record to date. We see precisely this behavior in unforced climate model control runs:
But in real world observations (from @BerkeleyEarth) we are seeing more records set over time. The green line is what we see in the real world, while the blue line is from unforced climate model control runs (and the orange line is what we'd expect given the 1/n rule):