Uncertainty in observational estimates of the aerosol direct radiative effect and forcing

Abstract

A lower-bound on the uncertainty in observational estimates of the aerosol direct radiative effect (DRE, the direct interaction with solar radiation by all aerosols), and the aerosol direct radiative forcing (DRF, the radiative effect of just anthropogenic aerosols, RFari), is quantified by making the optimistic assumption that global aerosol observations can be made with the accuracy found in the Aerosol Robotic Network (AERONET) sun photometer retrievals. The global mean all-sky aerosol DRE uncertainty was found to be 1.1 Wm-2 (1 standard deviation). The global mean all-sky aerosol DRF (RFari) uncertainty was determined to be 0.31 Wm-2. The total uncertainty in both quantities is dominated by contributions from the aerosol single scattering albedo uncertainty. These uncertainty estimates were compared to a literature survey of mostly satellite-based aerosol DRE/DRF values. Comparisons to previous studies reveal that most have significantly underestimated the aerosol DRE uncertainty. Past estimates of the aerosol DRF uncertainty are smaller (on average) than our optimistic observational estimates, including the aerosol DRF uncertainty given in the Intergovernmental Panel on Climate Change (IPCC) fifth assessment report (AR5). This disconnect between our observation-based uncertainty and that found in past aerosol DRF studies that rely, at least in part, on modeling is discussed. Also quantified is a potential reduction in the current observational uncertainty possible with a future generation of satellite observations that would leverage aerosol typing and more refined vertical information.