We know how the planets behave in relation to the sun and to each other today, but venturing millions or billions of years into the past, it can be tricky to figure out
what orbital changes may have impacted the Earth's climate.
Not exact matches
He then uses
what information is available to quantify (in Watts per square meter)
what radiative terms drive that temperature
change (for the LGM this is primarily increased surface albedo from more ice / snow cover, and also
changes in greenhouse gases... the former is treated as a forcing, not a feedback; also, the
orbital variations which technically drive the process are rather small in the global mean).
So albedo
change (owing to
changes in
orbital forcing, which is
what melts the ice sheets) was comparable to, and probably larger than, the CO2
change.
Christy et al provide descriptions of
what they
changed due to
orbital adjustments or overlaps as opposed to tracking surface temps and krigging between thousand mile apart un measured projected temps.