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Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing
Coupled climate model Holocene cooling events oceanic feedback solar forcing
2008/11/11
The coupled global atmosphere-ocean-vegetation model ECBilt-CLIO-VECODE is used to perform transient simulations of the last 9000 years, forced by variations in orbital parameters, atmospheric greenho...
Coupled climate model simulation of Holocene cooling events：oceanic feedback amplifies solar forcing
coupled global atmosphere-ocean-vegetation model ECBilt-CLIO-VECODE atmospheric greenhouse gas total solar irradiance
2008/11/10
The coupled global atmosphere-ocean-vegetation model ECBilt-CLIO-VECODE is used to perform transient simulations of the last 9000 years, forced by variations in orbital parameters, atmospheric greenho...
The origin of the major ice-sheet variations during the last 2.7 million years is a long-standing mystery. Neither the dominant 41 000-year cycles in δ18O/ice-volume during the late Pliocene and early...