Modelling of mineral dust for interglacial and glacial climate conditions with a focus on Antarctica

The East Siberian Ice Sheet loses mass by surface melt along all margins except for the Arctic Ocean coast, where the losses occur by calving and shelf basal melt only.. Further

While the changes of summer monsoon over South Asia and south- ern China are mainly controlled by global climate conditions (e.g. warmer sea surface temperature), the summer

The com- bination of cooler SSTs, an enhanced subduction of AABW and the reduction in export production in experiment O-LGM dramatically increased the oxygen content in both the

to solve underestimation of the simulated dust deposition over the Antarctic through, for example, detailed sensitivity experiments for analyzing what important factors are to

Therefore, in order to understand changes in the position and strength of ARC during the last glacial–interglacial cycle, here we reconstruct hydrographic changes in the

and Marsiat, I.: Simulations of the Northern Hemisphere through the last glacial- interglacial cycle with a vertically integrated and a three-dimensional thermomechanical ice-

In the Southern Hemisphere, the seasonal maximum and minimum of net chemical production appear in austral summer and win- ter, respectively, and the phasing of the H 2 seasonal cycle

Our model results indicate that sea-level changes during glacial-interglacial cycles affect the displacement and stress field in the forearc, along the plate interface, and in the