Not exact matches
The impact is a function of the magnitude of the change in the
concentration (i.e. deviation from the
average) of
aerosols.
However, over long time periods, the variation of the global
average temperature with CO2
concentration depends on various factors such as the placement of the continents on Earth, the functionality of ocean currents, the past history of the climate, the orientation of the Earth's orbit relative to the Sun, the luminosity of the Sun, the presence of
aerosols in the atmosphere, volcanic action, land clearing, biological evolution, etc..
The annual
average is about 0.25 of the peak — but you expect as well that the reflected SW would not vary as much as you suggest albedo of oceans being influenced by «solar zenith angle, wind speed, transmission by atmospheric cloud /
aerosol, and ocean chlorophyll
concentration.»
In response to increasing
concentrations of greenhouse gases and tropospheric sulfate
aerosols, the multimodel
average exhibits a positive annular trend in both hemispheres, with decreasing sea level pressure (SLP) over the pole and a compensating increase in midlatitudes.
The 2007 Fourth Assessment Report compiled by the IPCC (AR4) noted that «changes in atmospheric
concentrations of greenhouse gases and
aerosols, land cover and solar radiation alter the energy balance of the climate system», and concluded that «increases in anthropogenic greenhouse gas
concentrations is very likely to have caused most of the increases in global
average temperatures since the mid-20th century».