Originally published on the CICERO, Center for International Climate Research,
CICERO is Norway’s foremost institute for interdisciplinary climate research.
Although large emissions cuts are urgently needed if we are to achieve the global climate goals, it may take decades before we can measure the effect of the reductions on global temperature evolution, a new study shows.
In the open-access study, published in the scientific journal Nature Communications on 7 July 2020, CICERO researchers Bjørn H. Samset, Jan S. Fuglestvedt and Marianne T. Lund have analysed how global warming will evolve under different assumptions on future emissions reductions.
Their results show that if we only use the Earth’s surface temperature to measure whether emissions cuts lead to a slow-down in global warming, we may need to wait for decades before we can establish with certainty the temperature effect of the reduced emissions.
This is partly because the Earth’s climate responds slowly to changes in emissions, and partly because of the substantial natural variability in annual mean temperatures.
Slow climate response to emissions cuts
“Human-induced climate change can be compared with a tank ship at high speed and in big waves. If you want the ship to slow down, you will put the engine in reverse, but it will take some time before you start noticing that the ship is moving more slowly. It will also rock back and forth because of the waves,” Samset explains.
Over the past 50 years, the Earth’s surface temperature has on average increased by 0.2°C every decade, mainly due to human induced emissions of greenhouse gases. But from one year to the next, there are also large variations which are on a similar scale.
If we are to reach the Paris Agreement ambition of limiting global warming to no more than 2°C – or less – the first step will be to slow down the warming process,” says Samset.
But although the necessary emissions reductions are effective from day one, it will take some time before we can measure this effect with certainty, he says.
In addition to being impacted by greenhouse gas emissions, the Earth’s climate is also characterised by a lot of natural variability. One of the main goals of this study was to find out how we can expect the global surface temperature to develop, taking both human-induced and natural factors into account, according to Samset.
Just like it took some time to establish that global warming is happening, we will need to have some patience before we can determine that the actions taken to limit global warming are having the desired effect,” he explains.
Probably at least 15 years until we can establish the temperature effect
Samset and his colleagues estimate that even for the most optimistic scenarios, there is a risk that it will not be possible to establish that the emissions cuts have had an impact on global warming before 2035. However, that does not mean that the emissions reductions are not having the desired effect, according to Samset.
The effects of climate cuts can be compared with those resulting from social distancing during an epidemic. They work from day one, but because of the incubation time, it will take some time before you can see the effect on the infection rates,” he says.
Similarly, all reductions in warming emissions will lead to less heat being absorbed, but it will take some time before we can measure this effect,” says Samset.
Luckily, there are other methods we can use instead. We can estimate emissions reductions very quickly, and if there is a slower increase in the amount of greenhouse gases in the atmosphere, we will see it,” he adds.
But for temperature, which is what we really care about – and which, among other things, has an impact on the increased frequency and severity of extreme weather – it will take decades before we will be able to measure the effect,” he says.
Methane and CO2 emissions cuts most efficient
The study has also analysed the effect of cutting one single type of emissions, such as methane, soot, or carbon dioxide (CO2), independent of the development of other greenhouse gas emissions.
Different emissions affect the climate in various ways, and some have a stronger and more rapid effect on global temperature than others. We wanted to study the effects over time of the various types of emissions seen together with natural fluctuations, and how much we have to gain from concentrating on cutting some specific types of emissions,” says Fuglestvedt.
By combining results from a large U.S. modelling project with their own analyses, the CICERO researchers involved in this study have developed a new method for assessing the impact of individual or combinations of targeted emissions cuts.
The human-induced emissions with the biggest impact on global warming are CO2 and methane. If these emissions are reduced very strongly, we will see the effect quickly. But if reductions follow more realistic pathways, it will unfortunately take longer,” says Fuglestvedt.
The component with the most rapid temperature effect is soot. Soot particles only stay in the atmosphere for a few days, and their impact on the climate after an emission cut is therefore short-lived, he says.
“Unfortunately, the net climate impact of soot is not very strong, so there is less to gain from cutting soot emissions,” Samset adds.
Reducing soot emissions across the globe is, however, crucial for improving air quality, and it is thus important to find out how cuts in soot emissions affect the temperature increase, according to Samset.
No temperature effect of emissions reductions during COVID-19 expected
As part of the study, the researchers have also analyzed what would happen if air pollutant emissions such as sulphur dioxide (SO2) were reduced significantly, similar to what happened during the coronavirus pandemic. Unlike soot, methane, and CO2, cutting SO2 emissions would in fact speed up global warming.
SO2 turns into sulphate particles in the atmosphere, and they have a cooling effect because they reflect sunlight,” Lund explains.
According to a previous study by CICERO, the cooling effect of sulphate currently in the atmosphere can be as strong as 0.5°C. Like soot, sulphate particles only remain airborne for a few days, and cutting SO2 emissions would therefore have a very rapid temperature effect.
Some commentators have therefore asked whether we would now be able to measure increased global warming as a result of the COVID-19 lockdowns. According to the new study, the answer is no.
If we were to cut all SO2 emissions, it would only take a few years before we would see an increase in the global warming rate,” says Lund.
That is very fast compared with the other types of emissions, but still slow enough for us not to expect any measurable effect even from the sharp reductions we’ve seen during the ongoing pandemic. The SO2 cuts in 2020 will simply be too small and short-term to be visible above the noise from natural variability,” she adds.
Curbing out expectations
The emissions cuts necessary to limit global warming in line with the goals of the Paris Agreement will require rapid, major changes in society, businesses, and the energy sector.
But although this must happen quickly, we still need to have realistic expectations about how long it will take before we see a temperature effect of these changes, according to the CICERO researchers.
We performed this study partly to remind us all that things will take time. Today, the Paris Agreement targets, and public attention, are mainly focused on the change in global surface temperature, but this is among the slowest responding measurements we have for the effect of emissions reductions,” says Samset.
This does not mean that the cuts are not having any effect. It simply means that we need to be patient. Climate change will continue for several decades. The challenge facing us now is how to limit global warming as much as possible, and as rapidly as possible,” he adds.
Graph below from: Delayed emergence of a global temperature response after emission mitigation, published in Nature Communication, by Bjørn H. Samset, Jan S. Fuglestvedt & Marianne T. Lund (2020)
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Time of emergence of a global mean surface temperature signal for idealized individual mitigation efforts of a range of short- and long lived climate forcers. The colored expanding bars show the evolution of a statistically significant signal (t-test, p < 0.05), from zero (minimum) to 32 (maximum) ensemble members. The circles show the first year when 66% (21 members) show significant signals. The error bars show the 25–75% range (8 and 24 significant members respectively). Nature Communications doi: 10.1038/s41467-020-17001-1