Impact of Dust Aerosol on Glacial–Interglacial Climate

The temperature anomaly and dust concentrations recorded from central Antarctic ice core records display a strong negative correlation. The dust concentration recorded from an ice core in central Antarctica is 50–70 times higher during glacial periods than interglacial periods. This study investigated the impact of dust aerosol on glacial–interglacial climate, using a zonal energy balance model and dust concentration data from an Antarctica ice core. Two important efects of dust, the direct radiative efect and dust-albedo feedback, were considered. On the one hand, the direct radiative efect of dust significantly cooled the climate during the glacial period, with cooling during the last glacial maximum being as much as 2.05℃ in Antarctica. On the other hand, dust deposition onto the ice decreased the surface albedo over Antarctica, leading to increased absorption of solar radiation, inducing a positive feedback that warmed the region by as much as about 0.9℃ during the glacial period. However, cooling by the direct dust efect was found to be the controlling efect for the glacial climate and may be the major influence on the strong negative correlation between temperature and dust concentration during glacial periods.