Soren wrote on Apr 16
th, 2010 at 2:26pm:
At any rate, the only variable you ever talk about is CO2. You mention others only to discount them. You treat CO2 as if it was the 'one ring to rule them all'. For a topic like climate that is at least 'reasonably complex', this is monomania.
Which other variables have I discounted?
I think we've discussed all the variables. What we're talking about is very specific - What are the effects of increasing atmospheric greenhouse gases and clearing mainly tropical rainforest?
You stated that CO2 is 'just' a minor greenhouse gas. Well it isn't - it's the second most important greenhouse gas overall after water vapour , and we've already agreed that it doesn't matter how much water vapour we put into the atmosphere, because it will just drop out as precipitation.
In fact, most of the change that's occurring is happening in a specific part of the upper atmosphere. At that particular altitude, the air is very dry, and CO2 takes over as the most important greenhouse gas. So in terms of changing temperature, CO2 is the most important variable. It's actually more complex than that. Once you get really high in the atmospheric column, some of the re-emitted infrared is transmitted into space, but a fair proportion is also emitted towards the earth. It's a very subtle effect, but it is understood.
The main factor that controls water vapour concentration is temperature. You've already agreed with that.
Therefore the next biggest greenhouse gas in terms of effect is CO2, followed by methane, then Nitrous oxide. Do you agree with that?
What other variables are you interested in? All the heat ultimately comes from the Sun, and the temperature increase is determined by two main factors - the incoming heat from the sun, and the outgoing blackbody radiation from the Earth. These two factors control the heat balance.
I'm sure you've seen the attached figure before. It shows the extent of the forcings, including natural and anthropogenic.
Now the solar irradiance plus all the other factors combined have actually led to a slight net decrease in forcing as you can see from the figure.
The radiated longwave radiation has also decreased over the last few decades, and we know why. Why do you think that is?
So nobody is saying that it's just CO2, except for the strawman that you have constructed. I'm not sure if it was this thread or another, but somebody made the comment that the forcing equation might hold under laboratory conditions. Basically the radiative forcing equation only applies specifically to the atmosphere. I could explain how it's derived, or provide a link, but I doubt if it would be of any benefit to do so. It's dependent on the structure of the atmosphere at different altitudes. Let's leave it at that.
The fact that you believe that it only applies in a laboratory speaks volumes.
To answer the question - how much of the warming was caused by anthropogenic greenhouse gases is a difficult one because of the amplifying effect of water vapour (as we've discussed ad nauseum)
If we take the total natural forcings, as I said before, you get a slight decrease over the last 50 years or so. So the actual warming contribution from anthropogenic greenhouse gases is a tad more than 100%.
We should also remember that a fair whack of the CO2 ends up in the ocean too. The effect we have seen takes that into account.