I'm not saying that human induced aerosols are not important, but saying that the contribution of Greenhouse Gases to recent warming trends is over 100% because aerosols are masking some of that warming is most certainly alarmist. In addition, aerosol forcing isn't understood all that well, and is probably one of the largest uncertainties in Climate Science. Aerosols have an impact, but my stance is that anthropogenic aerosols are likely not as significant as you assert.
For example, the average lifespan of an anthropogenic aerosol is quite a bit less than the average lifespan of a molecule of CO2, and thus the effects from aerosols are likely to be much more local than the effects from CO2. Most of the anthropogenic aerosols are found in the Northern Hemisphere as a result of this local effect.
Yet, the Northern Hemisphere has actually warmed faster than the Southern Hemisphere according to both satellite measurements and surface temperature measurements. While this doesn't disprove an effect from aerosols, it suggests that the forcing from aerosols may lean more towards 0 in the IPCC's aerosol error range.
Also, do you deny that a significant increase in SW radiation has been absorbed at the Earth's surface over the last 30 or so years? This would seem to suggest that anthropogenic aerosols have not masked much warming during the late-20th Century warm period.
http://www.atmos-chem-phys.net/13/8505/2013/acp-13-8505-2013.html
From the paper:
"The 340 nm LER is highly correlated with cloud and aerosol cover because of the low surface reflectivity of the land and oceans (typically 2 to 6 RU, reflectivity units, where 1 RU = 0.01 = 1.0%) relative to the much higher reflectivity of clouds plus nonabsorbing aerosols (typically 10 to 90 RU). Because of the nearly constant seasonal and long-term 340 nm surface reflectivity in areas without snow and ice, the 340 nm LER can be used to estimate changes in cloud plus aerosol amount associated with seasonal and interannual variability and decadal climate change. The annual motion of the Intertropical Convergence Zone (ITCZ), episodic El Niño Southern Oscillation (ENSO), and latitude-dependent seasonal cycles are apparent in the LER time series. LER trend estimates from 5° zonal average and from 2° × 5° , latitude × longitude, time series show that there has been a global net decrease in 340 nm cloud plus aerosol reflectivity. The decrease in cos2(latitude) weighted average LER from 60° S to 60° N is 0.79 ± 0.03 RU over 33 yr, corresponding to a 3.6 ± 0.2% decrease in LER. Applying a 3.6% cloud reflectivity perturbation to the shortwave energy balance partitioning given by Trenberth et al. (2009) corresponds to an increase of 2.7 W m−2 of solar energy reaching the Earth's surface and an increase of 1.4% or 2.3 W m−2 absorbed by the surface, which is partially offset by increased longwave cooling to space."