A little extra carbon dioxide in the air may, unfortunately, go further towards warming Earth than previously thought. A team of British and U.S. researchers have uncovered evidence that Earth’s climate may be up to 50 percent more sensitive to long-term increases in atmospheric carbon dioxide than current climate models predict. The reason for the underestimation, they say, may be due to long-term changes in ice sheets and vegetation that are not well represented in today’s global climate models.
This is seems similar to Hansen’s argument for higher climate sensitivity, and if true is quite worrying. It means that ultimately greenhouse gas concentrations have to be brought to a lower level (Hansen says 350ppm, which will be a huge challenge given that we are already at 390ppm).
Just how much will global temperature rise in response to increases in atmospheric carbon dioxide? This is one of the key questions that climate scientists need to answer. According to the climate models used in the most recent report from the Intergovernmental Panel on Climate Change (IPCC), doubling the amount of carbon dioxide in the atmosphere from pre-industrial levels is expected to warm Earth by about 3 degrees Celsius (5 degrees Fahrenheit), once the atmosphere and oceans spend a few years or decades adjusting and reaching a balance.
But according to a recent study by a team of researchers that includes Gavin Schmidt of NASA’s Goddard Institute for Space Studies, Earth’s climate is also influenced by other, much slower processes. These include changes in ice sheets, vegetation and aerosols, for example, that take place over hundreds and thousands of years. Because of their complexity and long timescales, these processes are almost impossible to integrate into today’s climate computer models. As a result, it has been difficult to know just what their effect on Earth’s climate sensitivity would be.
To learn more about this sensitivity, Schmidt and his co-authors looked back 3 million years into Earth’s past. They used a computer model that describes the oceans and atmosphere to predict, retroactively, the climate of the mid-Pliocene — a period when both global temperatures and atmospheric carbon dioxide concentrations were higher than today. The model substantially underestimated just how high temperatures would go. When the researchers adapted the model to include the effects of long-term climate changes in vegetation and ice sheets, they were able to get a much closer representation of the warming in the Pliocene era.
The team found that it took much lower concentrations of atmospheric carbon dioxide to recreate the Pliocene’s warm climate than current models — which consider only the relatively fast-adjusting components of the climate — predict. Pliocene carbon dioxide levels are estimated to have been around 400 parts per million by volume (ppmv), while according to current simulations it would take 500 to 600 ppmv of carbon dioxide to bring about the warm temperatures of the Pliocene. As a result, the researchers estimate that Earth’s response to elevated concentrations of atmospheric carbon dioxide is 30 to 50 percent greater than previously calculated. In other words, the climate is more sensitive to carbon dioxide than we thought.
This higher sensitivity of the climate should be taken into account, the team concludes, when targets are set for limiting greenhouse gas emissions. The results of the study appear in Nature Geoscience.
Quantifying the equilibrium response of global temperatures to an increase in atmospheric carbon dioxide concentrations is one of the cornerstones of climate research. Components of the Earth’s climate system that vary over long timescales, such as ice sheets and vegetation, could have an important effect on this temperature sensitivity, but have often been neglected. Here we use a coupled atmosphere–ocean general circulation model to simulate the climate of the mid-Pliocene warm period (about three million years ago), and analyse the forcings and feedbacks that contributed to the relatively warm temperatures. Furthermore, we compare our simulation with proxy records of mid-Pliocene sea surface temperature. Taking these lines of evidence together, we estimate that the response of the Earth system to elevated atmospheric carbon dioxide concentrations is 30–50% greater than the response based on those fast-adjusting components of the climate system that are used traditionally to estimate climate sensitivity. We conclude that targets for the long-term stabilization of atmospheric greenhouse-gas concentrations aimed at preventing a dangerous human interference with the climate system should take into account this higher sensitivity of the Earth system.
Since these contributions to warming are slow, we will likely be able to overshoot the long term maximum safe level of greenhouse gasses as long as we eventually bring the atmospheric concentrations down bellow the upper safe limit. The real question is how long do we have to accomplish this?
I don’t think anyone has an answer yet.