North Atlantic Intermediate Depth Variability During the Younger Dryas: Evidence from Benthic Foraminiferal Mg/Ca and the Gfdl R30 Coupled Climate Model
- Andreas Schmittner,
- John C. H. Chiang,
- Sidney R. Hemming
Published Online: 19 MAR 2013
Copyright 2007 by the American Geophysical Union.
Ocean Circulation: Mechanisms and Impacts - Past and Future Changes of Meridional Overturning
How to Cite
Came, R. E., Curry, W. B., Oppo, D. W., Broccoli, A. J., Stouffer, R. J. and Lynch-Stieglitz, J. (2013) North Atlantic Intermediate Depth Variability During the Younger Dryas: Evidence from Benthic Foraminiferal Mg/Ca and the Gfdl R30 Coupled Climate Model, in Ocean Circulation: Mechanisms and Impacts - Past and Future Changes of Meridional Overturning (eds A. Schmittner, J. C. H. Chiang and S. R. Hemming), American Geophysical Union, Washington, D. C.. doi: 10.1029/173GM16
- Published Online: 19 MAR 2013
- Published Print: 1 JAN 2007
Print ISBN: 9780875904382
Online ISBN: 9781118666241
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