Global fine-mode aerosol radiative effect, as constrained by comprehensive observations
- 1Division of Atmospheric Science, Desert Research Institute, Reno, NV 89512, USA
- 2Dept. Atmospheric Sciences, Pusan National University, Busan 46241, South Korea
- 3Washington State University, Pullman, WA 99164, USA
- 4Royal Netherlands Meteorological Institute, 3730 AE De Bilt, the Netherlands
- 5National Meteorological Satellite Center, 27803, South Korea
- 6Dept. Civil and Environmental Engineering, Carnegie Mellon University, Pittsburgh, PA 15213, USA
Abstract. Aerosols directly affect the radiative balance of the Earth through the absorption and scattering of solar radiation. Although the contributions of absorption (heating) and scattering (cooling) of sunlight have proved difficult to quantify, the consensus is that anthropogenic aerosols cool the climate, partially offsetting the warming by rising greenhouse gas concentrations. Recent estimates of global direct anthropogenic aerosol radiative forcing (i.e., global radiative forcing due to aerosol–radiation interactions) are −0.35 ± 0.5 W m−2, and these estimates depend heavily on aerosol simulation. Here, we integrate a comprehensive suite of satellite and ground-based observations to constrain total aerosol optical depth (AOD), its fine-mode fraction, the vertical distribution of aerosols and clouds, and the collocation of clouds and overlying aerosols. We find that the direct fine-mode aerosol radiative effect is −0.46 W m−2 (−0.54 to −0.39 W m−2). Fine-mode aerosols include sea salt and dust aerosols, and we find that these natural aerosols result in a very large cooling (−0.44 to −0.26 W m−2) when constrained by observations. When the contribution of these natural aerosols is subtracted from the fine-mode radiative effect, the net becomes −0.11 (−0.28 to +0.05) W m−2. This net arises from total (natural + anthropogenic) carbonaceous, sulfate and nitrate aerosols, which suggests that global direct anthropogenic aerosol radiative forcing is less negative than −0.35 W m−2.