Model studies for climate change between the Holocene and the Pliocene, when Earth was about 3 °C warmer, find that slow feedbacks due to changes of ice sheets and
vegetation cover amplified the fast feedback climate response by 30 — 50 % [216].
Model studies for climate change between the Holocene and the Pliocene, when Earth was about 3 °C warmer, find that slow feedbacks due to changes of ice sheets and
vegetation cover amplified the fast feedback climate response by 30 — 50 % [216].