The Antarctic ice sheet and the triggering of deglaciations

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The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles (2011, background): “…but rather represent internal oscillations in the climate-cryosphere (Gildor and Tziperman, 2001) or climate-cryosphere-carbonosphere system (e.g. Saltzman and Maasch, 1988; Paillard and Parrenin, 2004), which can be synchronized (phase locked) to the orbital forcing (Tziperman et al., 2006).”
The polar ocean and glacial cycles in atmospheric CO2 concentration (2010, background): “Because the energy required for mixing two waters increases with the waters’ density difference, extremely dense ice-age Antarctic-sourced abyssal water may have mixed with overlying waters much more slowly than does modern Antarctic-sourced deep water 56,58 .”