J
JasonSB
Guest
Of course it does.Accepting this hypothesis - That would require / hold true, for ALL GHE’sIncluding water vapor
Now ask yourself this: why, then, would scientists classify CO2 as the dominant climate forcing greenhouse gas, but water vapour as only a climate feedback?
Are scientists really so stupid that this never occurred to them? That someone on a blog could overturn decades of research by asking a really obvious question?
If you come to what I hope is the obvious conclusion that that’s pretty unlikely and start to wonder, therefore, that there must be something else to explain it, you might actually realise for yourself that the answer is “Residence Time Matters”.
If I release a molecule of any greenhouse gas into the atmosphere, the impact that will have on the climate depends on both how potent it is and how long it will stay in the atmosphere. (Note that the individual molecule doesn’t matter, it’s the increase in the total number of molecules that counts. That individual molecule could get sucked straight up by a plant, for example, but because the plant sucked up that particular molecule it didn’t suck up another molecule that it otherwise would have, and so the increase in the total number of molecules is what persists.)
As an analogy, imagine you have an interest-bearing savings account. You earn more interest the more money you have in there, and you earn more interest the longer you leave it in there. (It also doesn’t matter which individual dollars go in and out of your account over time, what matters is the total during that time.)
So, clearly, the residence time for a greenhouse gas (and, in particular, the residence time for the increase in concentration, not the particular molecules) makes a difference, just like the length of time you leave money in your savings account does.
Now, it turns out that water has a very short residence time – it rains if there is more water in the atmosphere than it “naturally” wants – while CO2 has a very long residence time. If you were somehow able to dump a vast quantity of moisture into the atmosphere today, the spike in water vapour concentration would cause temporary warming but it would have all rained out again in a matter of weeks – far too short a time for it to affect the climate. (It would certainly make for some very wet weather, however.)
In contrast, if you dump a vast quantitiy of CO2 into the atmosphere – as we are doing now – then it will stick around for a very long time. (A significant portion will remain for centuries.) The whole time it is up there it is causing warming. Therefore releasing CO2 can force the climate to change, while releasing H2O would not.
The reason water is still a problem, however, is that the amount of water that the atmosphere “naturally” wants to hold is a function of the temperature of the atmosphere. If you raise the temperature, evaporation will increase, and the total amount of water vapour in the atmosphere will be higher, and it will stay higher as long as the atmosphere remains warmer. Because you have now found a way to raise water vapour levels for a long time, water vapour now has a chance to influence climate – and therefore acts to amplify the initial warming that you introduced with CO2.
So you can influence climate with CO2 directly, but you can only cause water vapour to influence climate indirectly, by triggering it as a feedback to the initial warming caused by a forcing, like CO2.