Lecture 15: Ocean chemistry Questions –How do the dynamics of the ocean affect the chemistry of the ocean, the distribution of biological activity, and.
Introduction AOGCM results and Eocene/PETM ocean circulation Hydrate modelling Conceptual model for hyperthermal orbital pacing A mechanism for the orbital.
Deep Ocean Monitoring : the East Sea (Sea of Japan) the East Sea (Sea of Japan) Kuh Kim 1, Kyung-Il Chang 1, Yun-Bae Kim 2 Jae-Hak Lee 3, Sang-Chul Hwang.
Are we leading to the fourth glacial period? Global Freezing- A review
GLOBAL FREEZING/GLOBAL COOLING.
Distribution of waters 71% of earth surface is ocean 4:1 in southern hemisphere 1.5:1 in northern hemisphere.
Atlantic Meridional Overturning Circulation (AMOC): Status, Requirements, and Issues Molly Baringer NOAA/AOML with contributions from B. Johns, C. Meinen,
Argo floats in the polar regions - technology, reality, future perspective Ilona Goszczko Institute of Oceanology Polish Academy of Sciences, Sopot, Poland.
Oceanography & Climate Synthesis Question: If all of the oceans currents changed direction, would they then heat the equator and cool the poles?
Albedo. 3/30 WHOT Teaching Point: Objective: Collect data on the albedo of various surfaces on Earth. Responsibilities: Albedo Lab Due Wednesday.
Numerical simulations of Rayleigh-Bénard systems with complex boundary conditions XXXIII Convegno di Fisica Teorica - Cortona Patrizio Ripesi Iniziativa.
A. Bozec 1, M. Kageyama 1, G. Ramstein 1, M. Crépon 2, L. Li 3 and P. Bouruet-Aubertot 2 1 - Laboratoire des Sciences du Climat et de l’Environnement/IPSL,