The ocean has absorbed more than 90% of the excess energy in the climate system over the past 50 years.
Speaker: Anja Slim (Monash)
How far downriver should waste-water be released to avoid contaminating an upstream water source? Using a shallow-water description of inertia-dominated, buoyancy-driven flow,
Speaker: Dr. Kraig Winters, Scripps Inst. of Oceanography and Dept. of Mech. and Aerospace Engr., UCSD
We consider stratified flows over isolated obstacles in the limit of strong stratification and tall obstacles for which the total kinetic energy of the flow is insufficient to d
DIMES: Diapycnal and Isopycnal Mixing in the Southern Ocean, and consequences for meridional overturning
Speaker: Sjoerd Groeskamp (UTas)
The global ocean circulation is of great importance for the earth’s climate system through its heat transport and the cycling and storage of CO2.