Similarly, a colder climate with generally decreased humidity q O could be closer to the critical threshold, which might be the reason for less - stable monsoon
circulations during glacial periods.
Not exact matches
*
Circulation changes in the Faeroe - Shetland Channel correlating with cold events
during the last
glacial period (58 - 10 ka).
In the past, major and rapid climatic variations which took place notably
during the last
glacial period (Heinrich
period) disturbed ocean
circulation.
Strong evidence from ocean sediment data and from modelling links abrupt climate changes
during the last
glacial period and
glacial - interglacial transition to changes in the Atlantic Ocean
circulation.