30 Mar 2012 09:00 - 10:00 Symposium Introduction and Paleoceanographic Perspective Edouard Bard The ocean and climate change : variations in ocean circulation 30 Mar 2012 09:00 - 10:00 Share Facebook Linkedin Copy url Audio-visual RSS
Friday 30 March 2012 Amphithéâtre Marguerite de Navarre, Site Marcelin Berthelot Open to all 09:00 - 10:00 Skip youtube video player Documents and media Download support pdf (1.44 MB) Speaker(s) Edouard Bard Professor at the Collège de France, CEREGE Aix-en-Provence Events Previous Symposium 30 Mar 2012 09:00 - 10:00 Edouard Bard Introduction and Paleoceanographic Perspective Symposium 30 Mar 2012 10:00 - 11:00 Gilles Reverdin Atlantic Surface Currents Symposium 30 Mar 2012 11:00 - 12:00 Harry Bryden Variability in the Deep Circulation of the North Atlantic Ocean Symposium 30 Mar 2012 14:00 - 15:00 Monika Rhein Changes in Water Mass Formation and Spreading Pathways in the North Atlantic Symposium 30 Mar 2012 15:00 - 16:00 Jochem Marotzke Predictability and Prediction of Atlantic Circulation and Climate Symposium 30 Mar 2012 16:30 - 17:30 Mathieu Rouault Hydrographic Data on the Agulhas Current in the Context of the Indian, Atlantic and Southern Ocean C… Symposium 30 Mar 2012 17:30 - 18:30 Arne Biastoch Modelling the Agulhas Current and Its Coupling with the Atlantic Circulation Next See also Edouard Bard, chair Climate and Ocean Evolution The ocean and climate change : variations in ocean circulation
Symposium 30 Mar 2012 11:00 - 12:00 Harry Bryden Variability in the Deep Circulation of the North Atlantic Ocean
Symposium 30 Mar 2012 14:00 - 15:00 Monika Rhein Changes in Water Mass Formation and Spreading Pathways in the North Atlantic
Symposium 30 Mar 2012 15:00 - 16:00 Jochem Marotzke Predictability and Prediction of Atlantic Circulation and Climate
Symposium 30 Mar 2012 16:30 - 17:30 Mathieu Rouault Hydrographic Data on the Agulhas Current in the Context of the Indian, Atlantic and Southern Ocean C…
Symposium 30 Mar 2012 17:30 - 18:30 Arne Biastoch Modelling the Agulhas Current and Its Coupling with the Atlantic Circulation
