Telltale history of AMOC of the final Northern Hemisphere deglaciation
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Video presentation at 2022 US AMOC Science Team Meeting
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.