The sensitivity of the Earth system to a doubling of atmospheric carbon dioxide may be twice as great as scientists had thought
By Alex Kirby
You may think the prospect of climate change is alarming, a call to action to slow down our emissions of carbon dioxide and other greenhouse gases.
Youâre almost certainly right. But some scientists are now suggesting you should be much more concerned than you are, because they think we may be seriously underestimating the problem.
The Geological Society of London (GSL) says the sensitivity of the Earthâs climate to CO2 could be double earlier estimates.
The Society has published an addition to a report by a GSL working party in 2010, which was entitled Climate change: Evidence from the Geological Record.
The addition says many climate models typically look at short term, rapid factors when calculating the Earthâs climate sensitivity, which is defined as the average global temperature increase brought about by a doubling of CO2Â in the atmosphere.
Scientists agree that a doubling of atmospheric CO2 levels could result in temperature increases of between 1.5 and 4.5Â°C, caused by rapid changes such as snow and ice melt, and the behaviour of clouds and water vapour.
But what the GSL now says is that geological evidence from palaeoclimatology (studies of past climate change) suggests that if longer-term factors are taken into account, such as the decay of large ice sheets, the Earthâs sensitivity to a doubling of CO2 could itself be double that predicted by most climate models.
Dr Colin Summerhayes, who led the statementâs working group, says: âThe climate sensitivity suggested by modern climate models may be fine for the short term, but does not encompass the full range of change expected in the long termâŚâ
But he cautions that there are really two âsensitivitiesâ involved: âClimate sensitivity is what happens in the short term in response to a doubling of CO2. But the Earth system sensitivity is what happens in the longer time frame as ice sheets slowly melt, and as sea level slowly rises.
ââŚThe IPCC focuses onâŚ the climate sensitivity â what will happen in the next 100 years. Earth system sensitivity tells you what happens in the next couple of hundred years after that.â
The GSLâs addition also reports new data showing that temperature and CO2 levels recorded in Antarctic ice cores increase at the same time. This, says Summerhayes, âmakes the role of CO2 in changing Ice Age climate highly significant.â
Atmospheric carbon levels are currently just below 400 parts per million (ppm) â a figure last seenÂ between 5.3 and 2.6 million years ago. Global temperatures were then 2-3Â°C higher than today, and sea levels were several metres higher, due to partial melting of the Antarctic ice sheet.
If the current rate of increase (2 ppm per year) continues, CO2 levels could reach 600 ppm by the end of this century; levels which, says Summerhayes, âhave not been seen for 24 million yearsâ.
Models match palaeoclimate
The new GSL statement outlines evidence that a relatively modest rise in atmospheric CO2 levels and temperature leads to significant sea level rise, with oceans more acidic and less oxygenated. Previous such events caused marine crises and extinctions, with the Earth system taking around 100,000 years to recover.
Dr Summerhayes said: âWe now have even more confidence from the geological record that the only plausible explanation for current warming is the unprecedented exponential rise in CO2 and other greenhouse gases.
âRecent compilations of past climate data, along with astronomical calculations, show that changes in the Earthâs orbit and axis cooled the world over the past 10,000 years. This cooling would normally be expected to continue for at least another 1,000 years.
âAnd yet Arctic palaeoclimate records show that the period 1950-2000 was the warmest 50 year interval for 2,000 years. We should be cool, but weâre not.â
He told Climate News Network: âThe main implication from my perspective is that the geological record tells us that increasing CO2 increases temperature, melts ice, and raises sea level. This we know independently of any fancy numerical model run by climate scientists.
âHowever, those climate scientistsâ models happen to come up with about the same answer as we get from the geological record, which suggests that the modellersÂ are likely to be on the right track.â
This article was produced by the Climate News Network