Telltale history of AMOC of the final Northern Hemisphere deglaciation
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Last deglaciation was indeed triggered by Northern Hemisphere insolation changes, amplified by albedo, CO2 and ocean circulation changes sea level rise
Climate model reproduces past abrupt climate change
TraCE-21K Project was made possible by the DOE INCITE computing program, and supported by NCAR, the NSF P2C2 program, and the DOE Abrupt Change and EaSM programs.