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Figure 4 also shows our estimates of the global radiative feedbacks.
Currently, atmospheric aerosols represent the largest source of uncertainty in global radiative forcing predictions3, especially in remote regions4.
The median global radiative forcing projections for high-emission RCPs is ~12 W m−2 (ref. 15).
Rugenstein, M. A. A., Caldiera, K. & Knutti, R. Dependence of global radiative feedbacks on evolving patterns of surface heat fluxes.
Methane (CH4) emissions and carbon uptake in temperate freshwater wetlands act in opposing directions in the context of global radiative forcing.
Aviation emission of gas phase pollutants and particulate matter contribute to global radiative forcing and regional air quality degradation near airports.
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Harries, J. E. & Belotti, C. On the variability of the global net radiative energy balance of the nonequilibrium Earth.
The difference in the local feedback parameters between low and high latitudes is the time-dependent global mean radiative feedback parameter.
Even worse, recent global BC radiative effect quantification[53] seems to be even higher than assumed by Jacobson[52] which would further increase above presented figures of an additional radiative effect of diesel car BC emissions in terms of CO2 equivalents.
Analysis of the simulation data of the first day leads to a deeper understanding of global teleconnections, radiative transfer and wave-coupling processes between the surface and the atmospheric layers.
The time variation of global mean radiative damping is therefore determined by the time-invariant local feedback parameter λ(r) and the time-varying spatial pattern of surface temperature change ΔT r,t).
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