Explained: Climate sensitivity

If we double the Earth’s greenhouse gases, how much will the temperature change? That’s what this number tells you.


This is the second part of an “Explained” on climate change. Part one dealt with radiative forcing.

Climate sensitivity is the term used by the Intergovernmental Panel on Climate Change (IPCC) to express the relationship between the human-caused emissions that add to the Earth’s greenhouse effect — carbon dioxide and a variety of other greenhouse gases — and the temperature changes that will result from these emissions.

Specifically, the term is defined as how much the average global surface temperature will increase if there is a doubling of greenhouse gases (expressed as carbon dioxide equivalents) in the air, once the planet has had a chance to settle into a new equilibrium after the increase occurs. In other words, it’s a direct measure of how the Earth’s climate will respond to that doubling.

That value, according to the most recent IPCC report, is 3 degrees Celsius, with a range of uncertainty from 2 to 4.5 degrees.

This sensitivity depends primarily on all the different feedback effects, both positive and negative, that either amplify or diminish the greenhouse effect. There are three primary feedback effects — clouds, sea ice and water vapor; these, combined with other feedback effects, produce the greatest uncertainties in predicting the planet’s future climate.

With no feedback effects at all, the change would be just 1 degree Celsius, climate scientists agree. Virtually all of the controversies over climate science hinge on just how strong the various feedbacks may be — and on whether scientists may have failed to account for some of them.

Clouds are a good example. Clouds can have either a positive or negative feedback effect, depending on their altitude and the size of their water droplets. Overall, most scientists expect this net effect to be positive, but there are large uncertainties.

“There is still lots of uncertainty in what the climate sensitivity is,” says Andrei Sokolov, a research scientist in MIT’s Center for Global Change Science, who has been doing research on climate sensitivity for many years. “Feedback is what’s driving things,” he says.

It is important to note that climate sensitivity is figured on the basis of an overall doubling, compared to pre-industrial levels, of carbon dioxide and other greenhouse gases. But the temperature change given by this definition of climate sensitivity is only part of the story. The actual increase might be greater in the long run because greenhouse gas levels in the atmosphere could more than double without strong policies to control emissions. But in the short run, the actual warming could be less than suggested by the climate sensitivity, since due to the thermal inertia of the ocean, it may take some time after a doubling of the concentration is reached before the climate reaches a new equilibrium.


Topics: Climate, Environment, Explained

Comments

The paleoclimate record demonstrates conclusively that the Medieval Warming Period was synchronous, world wide and had temperatures greater than we are experiencing today. How does Sensitivity explanation explain that?
The MWP was not worldwide. It was not warmer than today. See http://www.skepticalscience.com/medieval-warm-period.htm
James Hansen said that if "long-term" feedbacks were taken into account, the 3 degrees becomes 6 degrees for a doubling of CO2. If Hansen is used, 2 deg and 350 ppm CO2 are about the same. The upper limit that humans are supposed to be able to adapt to. Also I've always seen it 3 deg +/- 1.5 deg which would give 1.5-4.5 for a doubling of CO2. I've never seen an uncertainty applied to the 6 deg - could it be +/-3.0? In summary, there are a lot of uncertainties when attempting to pin down the sensitivity of our climate to CO2. It's hard to know the correct answer when we've never been there before. If we look at past recordings of several (3) million years ago as Dan Lunt of U. of Bristol did, then 100 ppm rise in CO2 would be somewhere aroung 3 deg. (Unfortunately both CO2 and Temp are given in ranges - the picture is fuzzy.)
The Medieval Warm Period was world wide in scope. It was warmer than today. Here's the picture of where the unequivocal peer reviewed evidence comes from. http://www.co2science.org/data/timemap/mwpmap.html Here's a link to the peer-reviewed papers. http://www.co2science.org/data/mwp/mwpp.php I'm still waiting for an explanation of how this Sensitivity explanation can be used to explain the MWP.
The case is not as definitive as Skeptical science presents it. There is some evidence that the MWP was both hotter than today and global. See http://hidethedecline.eu/pages/posts/medieval-warm-period-rdquomwprdquo-38.php and http://joannenova.com.au/2009/12/fraudulent-hockey-sticks-and-hidden-data/ also http://wattsupwiththat.com/2010/03/17/medieval-warm-period-seen-in-western-usa-tree-ring-fire-scars/
This is not a botany/agriculture problem. Would you see a chiropractor for a root canal?
Back to the top