Not exact matches
Overall forcing at the TOA is negative
averaged over all
aerosols, but significant
atmospheric heating and a net positive TOA forcing is possible for
aerosols with a strong black carbon component, and some of this will eventually be transmitted to the surface despite the reduction in surface insolation from the light scattering and absorptive properties of the
aerosols.
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.»
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».