Glacial Isostatic Adjustment Derived Boundary Conditions for Paleoclimate Simulation: the Refined ICE-6G_D (VM5a) Model and the Dansgaard-Oeschger Oscillation

W Richard Peltier, University of Toronto, Physics, Toronto, ON, Canada, Guido Vettoretti, University of Toronto, Toronto, ON, Canada and Donald F Argus, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, United States
Back to: Glacial Isostasy, Sea Level, and Earth System Evolution I