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Nature|April 1, 2005
Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulationAndreas SchmittnerNature|November 21, 2008
Glacial greenhouse-gas fluctuations controlled by ocean circulation changesAndreas Schmittner, Eric D GalbraithScience (New York, N.Y.)|February 2, 2002
Instability of glacial climate in a model of the ocean- atmosphere-cryosphere systemAndreas Schmittner, Masakazu Yoshimori, Andrew J WeaverNature|December 13, 2016
Centennial-scale Holocene climate variations amplified by Antarctic Ice Sheet dischargePepijn Bakker, Peter U Clark, Nicholas R Golledge, et al.Science (New York, N.Y.)|November 26, 2011
Climate sensitivity estimated from temperature reconstructions of the Last Glacial MaximumAndreas Schmittner, Nathan M Urban, Jeremy D Shakun, et al.Nature|April 7, 2012
Global warming preceded by increasing carbon dioxide concentrations during the last deglaciationJeremy D Shakun, Peter U Clark, Feng He, et al.Nature Communications|March 22, 2019
Deep-water circulation changes lead North Atlantic climate during deglaciationFrancesco Muschitiello, William J D'Andrea, Andreas Schmittner, et al.Proceedings of the National Academy of Sciences of the United States of America|August 3, 2011
Ice-shelf collapse from subsurface warming as a trigger for Heinrich eventsShaun A Marcott, Peter U Clark, Laurie Padman, et al.Science (New York, N.Y.)|October 2, 2020
Phasing of millennial-scale climate variability in the Pacific and Atlantic OceansMaureen H Walczak, Alan C Mix, Ellen A Cowan, et al.Scientific Data|March 10, 2023
A global synthesis of high-resolution stable isotope data from benthic foraminifera of the last deglaciationJuan Muglia, Stefan Mulitza, Janne Repschläger, et al.Pageof 1