Revkin has leading system dynamics expert Sterman on NOAA's 1,000-years-of-hell paper
I am a big fan of MIT’s John Sterman, one of the world’s leading experts on systems thinking.
In a post on “The Greenhouse Effect and the Bathtub Effect,” Andrew Revkin notes that Sterman’s work trying to reduce the biggest source of climate confusion is related to the new NOAA-led paper that I discussed here: Climate change “largely irreversible for 1000 years,” with permanent Dust Bowls in the Southwest and around the globe.
The bathtub analogy is that while atmospheric concentrations (the total stock of CO2 already in the air) might be thought of as the water level in the bathtub, emissions (the yearly new flow into the air) are the rate of water flowing into a bathtub. We need to lower the level, not just the flow. A great video clarifying the issue is here. It is narrated by my friend Andrew Jones. If you want to play the simulation itself, go here.
Revkin got Sterman’s comments on the paper, which I am reposting below:
I have read the Solomon paper.
It’s an excellent demonstration of the bathtub principle — the concept of stocks and flows, which prior research shows many people, even many highly educated people, don’t understand. Our mental models suggest that if we stop the growth of emissions, we will stop global warming, and if we cut emissions, we’ll quickly return to a cooler climate. We tend to think that the output of a process should be correlated with — look like — its input. If greenhouse gas emissions are growing, we think, the climate will warm, and if we cut emissions, we imagine that the climate will cool. In systems with significant accumulations, however, such correlational reasoning does not hold. Rather, it’s more like filling a bathtub. The amount of carbon dioxide in the atmosphere is like the level of water in a bathtub. The level grows as long as you pour more water in through the faucet than drains out. Right now, we pour about twice as much CO2 into the atmospheric tub than is removed on net by natural processes.
Stabilizing atmospheric concentrations requires emissions to fall to the net removal rate. Further, because of the processes highlighted in the Solomon paper and other analyses, including the IPCC AR4, the net removal of CO2 from the atmosphere is likely to fall as the stocks that absorb all that carbon, particularly the oceans, fill up. There are other key “bathtubs” — accumulations — that contribute to the irreversibility of climate change Solomon highlights. First, global mean surface temperature depends on the quantity of heat stored at the surface of the earth (earth, lower atmosphere, and the mixed layer of the oceans). That stock of heat is increased by net radiative forcing, the difference between the flow of energy coming in (primarily from the sun) less the flow of energy radiated back to space and the flow of heat transfered to the deep ocean. Today that inflow exceeds the outflow, so the average temperature is rising. Stabilizing the concentration of greenhouse gases in the atmosphere may stop the growth in net radiative forcing, but will not reduce the net inflow of energy (net radiative forcing) to zero. So temperatures will continue to rise until the planet warms enough to restore radiative balance. Solomon’s paper points out that the heat currently absorbed by the oceans does not disappear, but eventually returns to warm the surface. Thus temperatures won’t fall quickly even if atmospheric GHGs peak and eventually drop. And so on. Land-based ice in glaciers and ice-sheets will keep contributing to sea level rise as long as melting exceeds snowfall accumulation; stopping the growth of temperature would not stop the net melting.
What all this means is that the rate at which the climate returns to “normal” — say, early 20th century conditions — is so slow that, for key factors like sea level, precipitation patterns, ice sheets, and so on, the flow out of the bathtub is very very slow. So climate is a bit like the national debt. The US federal deficit has exploded in recent years, and the national debt has exploded as well. But suppose we could instantly cut the deficit to zero — drop it from about a trillion dollars per year to zero. What would happen to the debt? Of course it would not fall, but would instead stop growing at its all time peak value. Because the drains out of the various bathtubs involved in the climate — atmospheric concentrations, the heat balance of the surface and oceans, ice sheet accumulations, and thermal expansion of the oceans — are small and slow, the emissions we generate in the next few decades will lead to changes that, on any time scale we can contemplate, are irreversible.
One more critical point: it’s important that people not react to Solomon’s work with despair. Yes, a certain amount of climate change, due to past emissions, is inevitable, and will not be reversible. But it would be tragic if people concluded that therefore there is nothing we can do, that it is futile to reduce emissions, and that therefore all efforts should shift to adaptation. To the contrary: if nothing is done to cut emissions, and soon, the climate our children and grandchildren will face will almost certainly be far less hospitable, and there will be no turning back. By the time we know for certain how bad it will be it will be too late to take any corrective action. The Solomon paper should finally bury the idea that we can wait and see. It further strengthens the case for immediate, strong mitigation. The good news is that it’s getting cheaper every day to cut carbon emissions. Through learning, scale economies, R&D, and other forms of innovation, new technologies for carbon-neutral renewable energy are becoming more available and less expensive. Each megawatt of solar or wind capacity we build lowers the cost of the next and the next — a positive feedback we need to strengthen if we are too avoid irreversible harm to the ability of the planet to sustain us.
Jay W. Forrester Professor of Management
Director, MIT System Dynamics Group
MIT Sloan School of Management
Donate now to support our work.