Earth’s climate is the result of a dynamical system that absorbs energy from the incoming solar radiation. Not all of this energy is absorbed, considering that clouds and Earth’s surface reflect part of this radiation towards space. Once absorbed, this energy is either re-emitted as Earth’s surface thermal radiation or transits in a great journey that shapes our weather systems across the world. But, as with the energy contained in the incoming solar radiation, not all of this energy necessarily exits the system at once. The ocean, the atmosphere and their circulation delay or expedite the emission of the energy towards space in the form of thermal radiation.
In equilibrium, the net energy from the absorbed solar radiation should equal the energy in the outgoing thermal radiation, resulting in a zero net accumulation of energy in the system. However, if the system is forced «externally», the equilibrium breaks and the system responds to get a new equilibrium. The paramount example of our time is the man-made forcing that introduces CO_2 into the atmosphere. The increased CO_2 concentration augments the opacity of the atmosphere to thermal radiation emitted by the surface of the Earth and reduces the energy emitted towards space in comparison to the energy absorbed by the system. Thus, there is a net imbalance of energy that, eventually, translates into an increase in surface temperature.
The increase in surface temperature intensifies the thermal radiation as if the Earth tries to cool down by emitting more energy to space to recover the balance. However, temperature increase also changes other variables in the system. Some changes promote even more the accumulation of energy in the system (e.g. increased atmospheric water vapour that opaques more the atmosphere to thermal radiation) or work against the imbalance (e.g. increased mixing of the atmosphere to cool down the surface and warm up the upper troposphere, increasing the outgoing thermal radiation). These mechanisms are known as feedbacks. The ones that intensify the energy imbalance are positive feedbacks, whereas the ones that oppose are known as negative feedbacks. The sum of all of them is the so-called climate feedback, which is negative (if it were positive, the Earth would be an unstable system).
The above picture should be definitive: man-made global warming is out of any question. On top of man-made climate change, we have natural forcing (solar, orbital, natural variability, volcanoes and the like). Still, the natural forcing during the historical period has not changed as much as man-driven forcing and can not explain the observed warming.
In the article that Thorsten Mauritsen and I wrote and that appeared last week online in the journal Nature Geoscience, we look into the estimates of the real Earth’s short- and long-term climate sensitivities to a doubling of CO_2 concentrations. These sensitivities are temperature changes due to a doubling of CO_2 concentration. With the climate responses, we can derive estimates of future warming. Since the climate response depends on the forcing, climate feedback, and the imbalance in the energy budget, our estimates of the quantity have uncertainties. Some of the components —such as man-driven CO_2 forcing— have a small uncertainty. Others —such as the net man-driven aerosol forcing, the cloud effects on the energy budget and the ocean’s heat uptake— have large uncertainties across the instrumental record (the 20th and 21st centuries). Aerosol forcing is usually negative, that is, tends to reduce the total forcing. Then, if the real aerosol forcing were more negative than our expected value, the total forcing would be weaker than thought. Thus, the real Earth’s sensitivity should be higher because it needed less total forcing than thought to attain an observed temperature change. Conversely, if the real forcing is less negative, then the total forcing is stronger. Thus, the sensitivity is lower, because it needed more forcing to attain the observed warming. Therefore, as you can see, uncertainty is the key reason for the continuous research on climate sensitivity. What we found in our paper is that we reduced the uncertainty in the estimates of the climate sensitivities by using the warming observed since the 1970s. This period has less uncertainty in the aerosol forcing. But also we found that the estimates are higher than found before, based on physical reasons. For the short-term climate sensitivity we found that it is 20 per cent higher than calculated previously (from 1.41 to 1.67 in our study). This higher value stems from the absorption of part of the forcing by the upper layers of the ocean, an effect that was not considered in the usual energy-budget calculations. For more on these results look at this link.