Quote AuldSoul:
NO ONE says 90% of even these 200 scientists believed CO 2 was the primary cause.
hmmm, well, not exactly I suppose; it's better than that, as presumably, 100% of them believe that there is a 90% certainty that currently observed climate change is predominately anthropogenic. I'm pretty sure those "proponents" you mention that Seeker4 was referring to are the scientist who just released the 2007 IPCC Fourth Assessment Report, from which I quote the following:
[snip]
7 In this Summary for Policymakers the following levels of confidence have been used to express expert judgments on the correctness of the underlying science: very high confidence at least a 9 out of 10 chance of being correct; high confidence about an 8 out of 10 chance of being correct. (See Box TS.1.1)
[snip]
The understanding of anthropogenic warming and cooling influences on climate has improved since the Third Assessment Report (TAR), leading to very high confidence 7 that the globally averaged net effect of human activities since 1750 has been one of warming, with a radiative forcing of +1.6 [+0.6 to +2.4] W m-2. (see Figure SPM-2). {2.3. 6.5, 2.9}
• The combined radiative forcing due to increases in carbon dioxide, methane, and nitrous oxide is +2.30 [+2.07 to +2.53] W m-2, and its rate of increase during the industrial era is very likely to have been unprecedented in more than 10,000 years (see Figures SPM-1 and SPM-2). The carbon dioxide radiative forcing increased by 20% from 1995 to 2005, the largest change for any decade in at least the last 200 years.{2.3, 6.4}
• Anthropogenic contributions to aerosols (primarily sulphate, organic carbon, black carbon, nitrate and dust) together produce a cooling effect, with a total direct radiative forcing of -0.5 [-0.9 to -0.1] W m-2 and an indirect cloud albedo forcing of -0.7 [-1.8 to -0.3] W m-2. These forcings are now better understood than at the time of the TAR due to improved in situ, satellite and ground-based measurements and more comprehensive modeling, but remain the dominant uncertainty in radiative forcing. Aerosols also influence cloud lifetime
and precipitation. {2.4, 2.9, 7.5}
• Significant anthropogenic contributions to radiative forcing come from several other sources. Tropospheric ozone changes due to emissions of ozone-forming chemicals (nitrogen oxides, carbon monoxide, and hydrocarbons) contribute +0.35 [+0.25 to +0.65] W m-2. The direct radiative forcing due to changes in halocarbons8 is +0.34 [+0.31 to +0.37] W m-2. Changes in surface albedo, due to land-cover changes and deposition of black carbon aerosols on snow, exert respective forcings of -0.2 [-0.4 to 0.0] and +0.1 [0.0 to +0.2] W m-2. Additional terms smaller than ±0.1 W m-2 are shown in Figure SPM-2. {2.3, 2.5, 7.2}
• Changes in solar irradiance since 1750 are estimated to cause a radiative forcing of +0.12 [+0.06 to +0.30] W m-2, which is less than half the estimate given in the TAR. {2.7}