Here we propose that increasing variablility within the past million yearsmay indicate that the climate system was approaching a second
climate bifurcation point, after which it would transition again to a new stable state characterized by permanent mid-latitude Northern Hemisphere glaciation.
Not exact matches
The proximity of the present - day
climate to the Stommel
bifurcation point, beyond which North Atlantic Deep Water formation can not be sustained, varies from less than 0.1 Sv to over 0.5 Sv.
A concern with «large»
climate changes (i.e., on the scale of snowball Earths or runaway greenhouses) is that there's
bifurcation (loosely, tipping
points) in the system.
If a frequency of sites spatially and of data collection over time can produce enough dynamically significant data
points to satisfy the requirements of Chaos (eg, antialiasing,
bifurcation), then we can know just how badly we are measuring the
climate, and whether some currently ontic variability is really aleatory, or may be semi-deterministic in some spans and scales if only we have enough granularity in our sampling.
Tipping
points in open systems:
bifurcation, noise - induced and rate - dependent examples in the
climate system
As shown in Sect. 2.2, this concern was bolstered by the possibility of a huge, highly nonlinear temperature drop if the
climate system reached the upper - left
bifurcation point of Fig. 1.
I usually add the postscript that dynamical systems theory implies extreme
climate sensitivity near
points of chaotic
bifurcation — suggesting that changing the composition of the atmosphere may not be entirely risk free.