Speaker: Dr John Finnigan, CSIRO
The origin of the coherent eddy structures in and above tall plant canopies in neutrally stratified flow has been known for some years to result from the hydrodynamic instabilit
Speaker: Andrew Gunn (UTAS)
Idealised analytical theory on the role of mixing and wind for ocean carbon with GCM comparison.
Speaker: Edward Doddridge, University of Oxford
The existence of eddy compensation in the Southern Ocean, in which an eddy induced overturning circulation largely compensates the Ekman driven overturning circulation, is widel
Speaker: Dr. Luke Bennetts, University of Adelaide
The marginal ice zone (MIZ) is the 10s to 100s of kilometres of partially ice-covered ocean, which sits between the open ocean and the quasi-continuous ice cover.
Speaker: Nicola Maher, UNSW
Effects of volcanism on tropical variability.