Mechanisms of abrupt climate change
"Why do glacial periods end abruptly?
Notice the saw-tooth shape of the Vostok record, with abrupt warmings followed by more gradual coolings. Warming at the end of glacial periods tends to happen more abruptly than the increase in solar insolation. There are several feedbacks that might be responsible for this. One is the ice-albedo feedback. Ice has a higher albedo (or reflectivity) than vegetation, soil, or water. Therefore, when ice is present, less solar radiation is absorbed by the surface, temperatures decrease, and the ice will persist. Once ice begins to melt and uncover land or water, more solar radiation will be absorbed by the surface, raising temperatures and causing even more ice to melt.
This effect might be greatest over the oceans because sea ice can melt much more quickly than large continental ice sheets. A possible feedback also exists with atmospheric CO2. The amount of atmospheric CO2 decreased during glacial periods, in part because more CO2 was stored in the ocean due to changes in either ocean mixing or biological activity, although vegetative feedbacks and the trapping of methane may also have played roles. This decreased the atmosphere's greenhouse effect and helped to maintain low temperatures. Once CO2 began to rise at the end of the glacial periods, however, the atmosphere's greenhouse effect increased and contributed to further warming."
Thermohaline Circulation
"Why did the thermohaline circulation change abruptly?
The Younger Dryas occurred during the transition from the last glacial period into the present interglacial (the Holocene). During this time, the continental ice sheets were rapidly melting. A pulse of this meltwater flowing into the North Atlantic (Figure 8) reduced the salinity and density of the surface ocean, causing a reduction in the rate of deepwater formation. As deepwater formation slowed, less warm water flowed north from the tropics and the North Atlantic became colder. Eventually, the meltwater flux slowed and other changes occurred, causing deepwater formation to increase. See Model of Abrupt Change in the Thermohaline."