Paleoclimate data also provide quantitative information about how
nominally slow feedback processes amplify climate sensitivity [51]--[52], [54]--[56], which also is important to our analyses.
Paleoclimate data also provide quantitative information about how
nominally slow feedback processes amplify climate sensitivity [51]--[52], [54]--[56], which also is important to our analyses.
Not exact matches
In contrast, the 1000 GtC scenario, although
nominally designed to yield a fast -
feedback climate response of ∼ 2 °C, would yield a larger eventual warming because of
slow feedbacks, probably at least 3 °C.