The climate change in this period is generally believed to be associated
with precessional changes in the distribution of solar radiation, which primarily affect land - sea temperature contrast, and give only a regional warming, plus an enhancement of certain monsoonal circulations.
Not exact matches
Raymo and Paillard have a good story about the 100KYr cycle arising from the modulation of the
precessional cycle by the changes in the Earth's orbital eccentricity, coupled
with some glacial dynamical effects which «rectify» the high frequency
precessional signal.
The surface of the oceans are always warmer than the depths of the oceans > If you change the mixing efficiency, by shifting atmospheric circulations
with solar
precessional cycle for example, the mixing efficiency changes and the regions where precipitation falls changes.
That shift coincides
with the southern hemisphere receiving higher TSI due to the
precessional cycle.