The evolution of deep-ocean flow speeds and δ13C under large changes in the Atlantic overturning circulation: Toward a more direct model-data comparison-Reference-Cited by-同舟云学术

The evolution of deep-ocean flow speeds and δ13C under large changes in the Atlantic overturning circulation: Toward a more direct model-data comparison

Published:2015-02 Issue:2 Volume:30 Page:95-117
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Bakker Pepijn¹²,Govin Aline³⁴,Thornalley David J. R.⁵,Roche Didier M.¹⁶,Renssen Hans¹

Affiliation:

1. Faculty of Earth and Life Sciences; VU University Amsterdam; Amsterdam Netherlands

2. Now at College of Earth, Ocean and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA

3. MARUM-Center for Marine Environmental Sciences; University of Bremen; Bremen Germany

4. Now at Institut Pierre-Simon Laplace/; Laboratoire des Sciences du Climat et de l'Environnement; UMR 8212, CEA-CNRS-UVSQ, Gif-sur-Yvette France

5. Department of Geography; University College London; London UK

6. Laboratoire des Sciences du Climat et de l'Environnement; Gif-sur-Yvette France

Funder

European Union's Seventh Framework programme

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

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5. Last Interglacial temperature evolution-A model inter-comparison;Bakker;Clim. Past.,2013b

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3. Anomalously weak Labrador Sea convection and Atlantic overturning during the past 150 years;Nature;2018-04

4. Atlantic deep water circulation during the last interglacial;Scientific Reports;2018-03-13