A new analysis of an ice core from Dome Fuji in Antarctica, along with
climate simulation results, shows a high degree of climate instability
(that is, rapid climate fluctuations) within glacial periods with
intermediate temperatures. This instability was attributed primarily to
global cooling caused by a reduced greenhouse effect.
Relationship between the frequency of climate fluctuations with
temperatures in the Antarctic during the past 720,000 years obtained
from analysis of Antarctic ice cores (black spots), as well as results
for the final glacial period based on ice cores from Greenland (red
squares). During the warm interglacial periods, and the coldest portion
of a glacial period, the frequency of climate fluctuations was low, but
during periods of intermediate temperatures within a glacial period,
climate fluctuations occurred frequently and the climate was unstable.
https://www.sciencedaily.com/releases/2017/05/170502095125.htm
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