I haven't been a political blogger, and I'm not about to start now. Yet the news of the past few days does offer ways to illustrate systems concepts I've mentioned before, and so I thought I'd point out what I hope is obvious to all here.
For but one example, take
US President Bush's goal of having greenhouse gas (GHG) emissions stop growing by 2025, which is
stirring up comment world-wide.
In
system dynamics terms, GHG emissions (largely CO
2) are a flow, and the amount of CO
2 in the atmosphere is a stock. If you recall what I've written before on stocks and flows, you'll see that stopping the increase of a flow does
not mean that the stock will decrease; it simply means that it will increase less rapidly.
In other words, even if we do meet this goal, things may well continue to get worse well after 2025, but they will at least get worse less rapidly after then.
I want to show you a little model that demonstrates that behavior, but, to publish it here, I'd like to get the numbers at least close to right, and that would take a bit of research time I don't have tonight. Let me try an analogy, instead; those of you who studied and remember the calculus can probably make a more elegant argument, and those who do system dynamics models can create one on your own in a few minutes (if you have the needed parameters, let me know, or post a pointer to your model).
In the real world, we are emitting CO
2 into the atmosphere by breathing, burning fossil fuels, and the like. That stock of CO
2 in the atmosphere is growing and
threatening climate havoc.
Some of that CO
2 is taken out of the atmosphere each year through the action of photosynthesis and perhaps other mechanisms.
According to the science I read, we have too much CO
2 in the atmosphere at present, and our global CO
2 emissions per year, already above what the environment can naturally purge, are increasing. If that weren't the case, there would be little reason for
President Bush's call to action.
Let's look at an analogous situation. For example, let's say you have a bathtub that's three-fourths full of water. The drain is open, but it's partially clogged, and so it's draining slowly.
In addition, the faucet is turned on, putting more water in the tub. It so happens that the water is currently coming into the tub faster than the partially-stopped drain can take it out, so the water level is rising, causing fears for the well-being of the bathroom floor.
The person controlling the faucet is
opening the faucet as we speak, letting water come into the tub at an ever faster rate. That person, realizing the risk to the floor, promises to stop opening the faucet anymore in about 15 minutes.
What do you think will happen to the floor?
Even with the rough data I supplied, I hope you can see that the water will rise increasingly rapidly for the next 15 minutes. If the person takes their hand off the faucet in 15 minutes, the water will continue to rise until it overflows the tub (assuming it doesn't overflow sooner). The only way to save the floor is to reduce the flow of water from the faucet to
below the flow of water out of the drain
before the tub overflows. Even if they started reducing the flow of water out of the faucet now, the water in the tub would still rise until the inflow was less than the outflow.
Of course, this is a silly little example; the real world of GHG emissions is much more complex. Yet the general principle of stocks and flows holds: as long as the inflow exceeds the outflow, the stock will rise.
I'm not about to use this short, informal essay to argue for or against specific GHG or climate proposals or to try to balance climate stability against economic stability. I
am suggesting that we all remember
the lesson of stocks and flows when we are thinking about or evaluating policies such as these.
PS: Thanks to colleague
Wayne Wakeland for, in a totally different situation, reminding me of the effectiveness of simple bathtub models (and I hope it worked here!).
Labels: environment, simulation, system dynamics, systems thinking