Just a few points to keep the record straight. There are actually a whole host of different radiative forcings affecting the climate, mostly positive, some negative. This is a fairly good graphical summary of the main ones.
You mention albedo changes due to ice sheets and vegetation. It’s important to note that albedo changes are in two distinct categories: forcings and feedbacks, and need to be kept separate because they’re fundamentally different. An albedo forcing is an independent factor that drives the climate in and of itself – the primary example is land use and land cover changes from human activity, which you’ll find in the above chart. Ice cover changes, however, are feedbacks that are a direct consequence of Arctic warming and which amplify that warming when ice cover is reduced. They’re like the increase in water vapor that amplifies CO2 warming. Because they’re feedbacks intrinsically tied to the underlying forcings, these things don’t appear on the chart, but they’re obviously of critical importance in computing and modeling how climate responds to forcings.
Good point about climate sensitivity. Climate sensitivity is the measure of how much a given level of forcing will actually change the global average temperature under specified conditions, and is essentially a computation of forcings and all associated feedbacks on the earth’s total energy balance; the most common measure is equilibrium climate sensitivity which is defined as the temperature increase at equilibrium resulting from a doubling of CO2. Yes, the fact that we can observe the effects of CO2 changes in the paleoclimate record helps us estimate ECS, but it’s not the only source of input. We also have extensive modeling runs, the modern instrumental record, and other sources that all have strengths and weaknesses.
As a side note, ECS is a temperature delta so its unit is °C, not W/m[sup]2[/sup] which is a unit of the underlying forcing. After decades of research and refinement its estimated value remains basically unchanged at about 2 to 4.5 °C with a most probable value of about 3°C.