R. Drummond coauthored the ICE-6G_C model of glacial isostatic adjustment. Station motions constrain former ice thickness and unloading, while time-dependent gravity and sea-level records test the resulting Earth response.[ref]
Space geodesy constrains ice age terminal deglaciation: The global ICE-6G_C (VM5a) model by W. R. Peltier and others. Abstract: geodetic refinement and independent validation
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