Publication | Open Access

Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores

Taylor DomeCarbon SequestrationIce-water SystemEngineeringDml Ice CoresCo 2CryosphereGeochemistryEarth System ScienceGlacial ProcessIce LoadPaleoclimatologyEarth ScienceEarth's Climate