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Antarctic Ice Sheet Vulnerable to AMOC-induced subsurface warming

Warming oceans could cause Antarctic Ice Sheet collapse, sea level rise

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Northern influence on southern deglaciation confirmed

Last deglaciation was indeed triggered by Northern Hemisphere insolation changes, amplified by albedo, CO2 and ocean circulation changes

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A new era of paleoclimate modeling

Climate model reproduces past abrupt climate change



TraCE-21KA Project

TraCE-21KA 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.