Laurent Li Laboratoire de Météorologie Dynamique (LMD) Institut Pierre-Simon Laplace (IPSL) CNRS, Université Pierre et Marie Curie (UPMC) 4, Place Jussieu,
Assessing the efficiency of iron fertilization on atmospheric CO2 using an intermediate complexity ecosystem model of the global ocean Olivier Aumont 1.
Physical / Chemical Drivers of the Ocean in a High CO 2 World Laurent Bopp IPSL / LSCE, Gif s/ Yvette, France.
Introduction AOGCM results and Eocene/PETM ocean circulation Hydrate modelling Conceptual model for hyperthermal orbital pacing A mechanism for the orbital.
Mercator Ocean newsletter 23
1 JongJin Park Woods Hole Oceanographic Institution Decay Time Scale of Mixed Layer Inertial Motions in the World Ocean (Observations from Satellite Tracked.
1 Using Satellite Data for Climate Modeling Studies: Representing Ocean Biology-induced Feedback Effect in the Tropical Pacific Rong-Hua Zhang CICS-ESSIC,
Instrumentation types, data and metadata (accuracy, biases and known issues) CTD problems/metadata J. Swift, UCSD Scripps Institution of Oceanography "The.
Argo Products at the Asia-Pacific Data-Research Center Konstantin Lebedev, Sharon DeCarlo, Peter Hacker, Nikolai Maximenko, James Potemra, Yingshuo Shen.
Brad deYoung Open Pelagic Ecosystems. Roadmap Ecosystem structure – considerations of the issues and how to think about them Regime shifts in the.
4th Annual CTB SAB Meeting ESSIC, UMD 11 September 2008
Define Current decreases exponentially with depth and. At the same time, its direction changes clockwise with depth (The Ekman spiral). we have,. and At.
