Zelandakh,
I know of no scientists who dispute the heat trapping capability of CO2 either, I just did not want to speak for everyone. The feedbacks are highly debatable, and is currently the largest area of dispute among scientists. I have seen very few (but some) who contend that the overall feedback is negative. This is due to saturation, interferences, and the small absorption of incoming solar radiation. The positive feedback is primarily due to water vapor; this is due to the increase in atmospheric water content due to the increase in temperature, but can influenced by the previously mentioned negative feedbacks. Currently, the biggest uncertainty is clouds. This effect is two-fold. First, increased clouds result in decreased water vapor, as the water condenses to form the clouds, reducing the positive water vapor feedback. Secondly, clouds reduce incoming solar radiation, leading to reduced warming. More scientists think that clouds will increase in a warming world due to the increased water content in the atmosphere. However, some think that the increased warmth will lead to a reduction in cloudiness. Recent data have suggested that the two are linked, but the generally thinking is that the reduced cloudiness leads to the temperature increase, not the other way around. This change in cloudiness is thought to be related to the oceanic cycles, but is still an area of contention. How the oceans react to increased warmth is not well understood.
Two other areas which are thought to have a measureable influence are aerosols and albedo. These two factors have more than one source. In the case of aerosols, some are manmade, some are terrestrial, and some are galactic. All research has shown that aerosols reduce incoming solar radiation from reaching the Earth's surface, but the effects on recent temperature changes have been challenged. Albedo changes are mostly manmade; urbanization, deforestation, and agriculture. Urbanization has decreased the Earth's albedo in many ways, leading to increase absorption of incoming solar radiation. Hence, deforestation to build cities leads to higher temperatures. Deforestation for agriculture has the opposite effect, as most crops have a higher albedo than the trees. However, irrigation can reduce the albedo significantly. Global warming can reduce the albedo also, as snow and ice melt, revealing dark land and water.
There is a wide disagreement as to the overall feedback effects. The laboratory results show a 1.1C temperature increase with a doubling of CO2. The first contentions are the negative atmospheric feedback. This value has been quoted as reducing the climate sensitivity by 10-50% (i.e. 0.6 - 1.0 C / doubling). The increase due to water vapor is fairly well known, and equal to ~75% of the initial temperature rise (assuming all the water vapor remains as vapor). The decrease due to water vapor condensing to form clouds has been been reported from negliglible to larger than the increase due to water vapor. Barton Paul Levenson summarized many of the studies which examined climate sensitivity, and found recent values ranging from 0.75 to 4.5 C/ doubling (earlier studies had a higher range).
http://bartonpaullev...ensitivity.html
Realclimate had a discussion about a recent paper which showed that the climate sensitivity based on paleoclimatic restraints since the last glacial maximum has a range of 1.7 - 2.6C/ doubling (1.2 - 2.9 at the 95% confidence level). The biggest issue with this correlation, is that this is based on a temperature/CO2 relationship at the cold end of the temperature spectrum, and may differ on the high end.
http://www.sciencema...t/334/6061/1385