KenJackson said:
Please critique this logic.
- It's well known from chemistry that cooler water can hold more gasses in solution than warmer water.
- As ocean temperatures rise (slowly, for any reason, over centuries) dissolved greenhouse gasses will come out of solution and into the atmosphere. Conversely, as ocean temperatures cool, more greenhouse gasses in the atmosphere will be dissolved.
- This action is positive feedback. That is, it only serves to make the existing trend worse instead of opposing it.
- Any system with primarily positive feedback is inherently unstable and will end up at one extreme or the other.
This logic seems to suggest that no matter what happens, the Earth is doomed to end up either scorched like Venus or frozen like Mars. And yet, as far as I'm aware, the Earth has been quite stable for eons. So what gives?
First, a correction - oceans currently at as a sink for CO2. This is because you're not only increasing the water temperature, but also partial pressure of atmospheric CO2, plus, the CO2 already in the oceans is removed by formation and sedimentation of carbonates, which reduces oceanic partial pressure of CO2.
A third, up to half of the anthropogenic CO2 emissions ends up in the oceans. (
https://www.gfdl.noaa.gov/bibliography/related_files/us9301.pdf)
It is feasible that at some point in the future, when ocean temperatures will have risen enough as compared to CO2 concentrations, so as to reach saturation, they will start to release their stored CO2.
So, currently, they don't act as positive feedback in this way (but they do act as one in the sense of being the source of water vapour).Anyway, even using some other positive feedback as an example - it doesn't mean that the system is inherently unstable, because there are also negative feedbacks. Forcings, and both types of feedbacks interact to produce new equilibrium point.
For one, the hotter you make the planet, the faster it re-radiates energy into space (as per the Stefan-Boltzman law), so at some point a new equilibrium point is reached. For a runaway destabilisation you'd need positive feedbacks to overcome all negative feedbacks, an stay there. This isn't true even on Venus or Mars, as neither has 0 K temperature, nor infinite temperature - their climates have stabilised at whatever the corresponding equilibrium temperature is.
As a rule of thumb, feedbacks can't be the driver of climate change. They need something else to force the change, to which they then respond.
That's why when referring to the causes of climate change, people talk only about the forcings (drivers).
Let's take the aforementioned water vapour as an example. It is a greenhouse gas much stronger than CO2. However, in the environment of Earth, water condenses, while CO2 doesn't. So, if we add extra water vapour emissions, they will not stay in the atmosphere, and drive the long-term temperature changes, but will instead precipitate within hours to days. Hence water vapour is not a climate forcing.
On the other hand, you can pump CO2 into the atmosphere practically without limit, which then causes temperature to rise, which causes more evaporation and more water vapour to stay in the atmosphere, which in turn causes more temperature increase - i.e., water vapour acts as positive feedback to CO2 forcing.
phyzguy said:
Since there have been forcing functions in the geologic past much larger than what we are currently doing, and since the Earth hasn't run away to either scorched Venus or frozen Mars,
To be fair, it is possible there were periods when Earth was frozen over (the snowball Earth hypothesis).