Speaker
Emile Deléage
(Université Grenoble Alpes)
Description
In this talk, I will present a system of partial differential equations that is used in climate models for the ocean-atmosphere interface. I will first explain some physical and mathematical assumptions that are used in the derivation of the model, and in particular the important role of turbulence parametrisation in the different boundary layers. I will then give some elements for the theoretical analysis of the corresponding problem.