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
Year: 2004
Type: article
Institutions: University of Bern, University of Washington, University of Texas Institute for Geophysics, The University of Texas at Austin, Centre National de la Recherche Scientifique, Institut des Géosciences de l'Environnement, Laboratoire de Glaciologie et Géophysique de l’Environnement, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDG: Climate action
Open Access status: closed
OpenAlex ID: W2168628932
