Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern
Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern
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Author / Creator
Zhang, Z.-S. , Nisancioglu, K. H. , Chandler, M. A. , Haywood, A. M. , Otto-Bliesner, B. L. , Ramstein, G. , Stepanek, C. , Abe-Ouchi, A. , Chan, W.-L. , Bragg, F. J. , Contoux, C. , Dolan, A. M. , Hill, D. J. , Jost, A. , Kamae, Y. , Lohmann, G. , Lunt, D. J. , Rosenbloom, N. A. , Sohl, L. E. and Ueda, H.
Publisher
Katlenburg-Lindau: Copernicus GmbH
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Language
English
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Publisher
Katlenburg-Lindau: Copernicus GmbH
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Contents
In the Pliocene Model Intercomparison Project (PlioMIP), eight state-of-the-art coupled climate models have simulated the mid-Pliocene warm period (mPWP, 3.264 to 3.025 Ma). Here, we compare the Atlantic Meridional Overturning Circulation (AMOC), northward ocean heat transport and ocean stratification simulated with these models. None of the models...
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Full title
Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern
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TN_cdi_doaj_primary_oai_doaj_org_article_a866fcbeeaa44094a7f644bf2f0d5b9b
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_a866fcbeeaa44094a7f644bf2f0d5b9b
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ISSN
1814-9332,1814-9324
E-ISSN
1814-9332
DOI
10.5194/cp-9-1495-2013