Small
changes in insolation driven by changes in the Earth's orbit can push the planet into or out of an ice age through the planet's «climate feedback» mechanisms.
These are thought to be driven by the large regional
changes in insolation driven by orbital changes.
Not exact matches
A 2000 - year transient climate simulation with the Community Climate System Model shows the same temperature sensitivity to
changes in insolation as does our proxy reconstruction, supporting the inference that this long - term trend was caused by the steady orbitally
driven reduction
in summer
insolation.
Gradual,
insolation -
driven millennial - scale temperature trends
in the study area were punctuated by several abrupt climate
changes, including a major transient event recorded
in all five lakes between 4.3 and 3.2 ka, which overlaps
in timing with abrupt climate
changes previously documented around the North Atlantic region and farther afield at w4.2 ka.
In the case of the 100 kyr ice age cycles, that forcing is high northern latitude summer insolation driven by predictable changes in Earth's orbital and rotational parameters — aka, Milankovitch theory — which has the intial effect of melting glaciers, thereby reducing albedo at those latitude
In the case of the 100 kyr ice age cycles, that forcing is high northern latitude summer
insolation driven by predictable
changes in Earth's orbital and rotational parameters — aka, Milankovitch theory — which has the intial effect of melting glaciers, thereby reducing albedo at those latitude
in Earth's orbital and rotational parameters — aka, Milankovitch theory — which has the intial effect of melting glaciers, thereby reducing albedo at those latitudes.
Observed temperature (black line), the out - of - sample forecast for global surface temperature
driven by anthropogenic
changes in radiative forcing (red line) and the out - of - sample forecast for global surface temperature
driven by natural variables (solar
insolation, SOI, and volcanic sulfates)(green line).
«The Milankovitch theory of climate
change proposes that glacial - interglacial cycles are
driven by
changes in summer
insolation at high northern latitudes [i.e., solar irradiance received].