Not exact matches
However, in the global mean, these changes sum to zero (or very close to it), and so the global mean sensitivity to global mean
forcings is huge (or even undefined) and not very useful to understanding the eventual
ice sheet growth or carbon cycle feedbacks.
Orbital
forcing causes
ice ages or ends them by redistributing incoming solar radiation over seasons and latitudes so that
ice sheet growth or decay is more or less favorable on a regional basis, with a resulting global average albedo feedback.)
Other
forcings, including the
growth and decay of massive Northern Hemisphere continental
ice sheets, changes in atmospheric dust, and changes in the ocean circulation, are not likely to have the same kind of effect in a future warming scenario as they did at glacial times.
«Changes in the CO2 and CH4 content have played a significant part in the glacial - interglacial climate changes by amplifying, together with the
growth and decay of the Northern Hemisphere
ice sheets, the relatively weak orbital
forcing»
The
growth and decay of continental
ice sheets represents a slow feedback operating over millennia; if one is concerned with the more rapid response of the climate to CO2,
ice sheets have to be accounted for as a major
forcing.