LEGI - UMR 5519

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Le jeudi 24 mai, le séminaire interne sera annulé pour que l’équipe MEIGE puisse participer à la journée ECOUFLU.
Le texte de l’annonce :
Comme vous le savez peut-être, les membres du plateau ECOUFLU (...)

Oceanic fine structure has been studied since the development of CTD and microstructure profilers allowed to resolve the vertical scales of temperature and salinity in the ocean. In the context (...)

In the present talk, Large Eddy Simulation of a Stably stratified Atmospheric Boundary Layer is performed. we focus on the specific role played by Görtler vortices in katabatic flows. A downslope (...)

Bistability, a striking property of some climate features, can be obtained in purely hydrodynamic systems in turbulent regimes and can be explained in terms of statistical mechanics. Here, we (...)

The Southern Ocean (SO) is home to some of the strongest of the world’s ocean currents. Recent observations and numerical experiments suggest that a fraction of the energy of SO currents is (...)

Gravity flows are ubiquitous in several geophysical and industrail contexts and play an important role in turbulent kinetic energy transfer, as well as in turbulent transport and mixing with (...)

A horizontal circular disc oscillating in a density-stratified fluid radiates internal gravity waves. Viscosity affects both the propagation of the waves through the fluid and their generation at (...)

2D turbulence is naturally defined as a turbulent flow depending only on two space coordinates x,y or qlternqtively qs flow confined to a surface (which does not need to be plane, for instance a (...)

2D turbulence is naturally defined as a turbulent flow depending only on two space coordinates x,y or qlternqtively qs flow confined to a surface (which does not need to be plane, for instance a (...)