Here are the contributions of the different radiative forcings, relative to pre-industrial times:
I think clouds are primarily a negative feedback since they increase albedo (as shown above). It would be silly to assume no feedbacks since temperature increase shifts equilibria toward the gaseous phase. But in general you are correct in saying the amount of feedback is one of the biggest areas of contention. Its very much a *hot* topic in climate research. From the climate sensitivity link in my last post:
The IPCC Fourth Assessment Report summarized climate sensitivity as "
likely to be in the range 2 to 4.5°C with a best estimate of about 3°C, and is very unlikely to be less than 1.5°C. Values substantially higher than 4.5°C cannot be excluded, but agreement of models with observations is not as good for those values."
Individual studies have put climate sensitivity from a doubling of CO2 at anywhere between 0.5°C and 10°C; however, as a consequence of increasingly better data, it appears that the extreme higher and lower values are very unlikely. In fact, as climate science has developed and advanced over time , estimates have converged around 3°C. A summary of recent climate sensitivity studies can be found
here.
A study led by Stefan Rahmstorf concluded "many vastly improved models have been developed by a number of climate research centers around the world.
Current state-of-the-art climate models span a range of 2.64.1°C, most clustering around 3°C" (Rahmstorf 2008). Several studies have put the lower bound of climate sensitivity at about 1.5°C,on the other hand, several others have found that a sensitivity higher than 4.5°C can't be ruled out.
A 2008 study led by James Hansen found that climate sensitivity to "fast feedback processes" is 3°C, but when accounting for longer-term feedbacks (such as ice sheet disintegration, vegetation migration, and greenhouse gas release from soils, tundra or ocean), if atmospheric CO2 remains at the doubled level, the sensitivity increases to 6°C based on paleoclimatic (historical climate) data.
How did you get 2 ppm/year? Im not sure what the current rate is but you cant extrapolate a linear trend since greenhouse gases are increasing exponentially (see post 2070). That's why climate sensitivity is expressed in terms of doubling CO2. Here's the IPCC projected CO2 levels for various scenarios:
Soo... not trying to come off as alarmist, but IMO it seems unlikely we'll be able to keep the temperature increase under 2 degrees (which is roughly the goal and best case scenario -see figure in previous post)