# LEGI - UMR 5519

Laboratoire des Écoulements Géophysiques et Industriels

## Search

Home > Teams > MEIGE team > Scientific communications > Group seminars

## Group seminars

Informal seminars (20 min of presentation, usually Thursday at 12am) are organized in the team.

Send an email to:
Eletta Negretti .

### Next seminars:

2019/01/09 Thursday 12h00- Eletta Negretti -

### List of all seminars:

Page(s) : < 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10

### Impact des ondes de relief dans la circulation océanique

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 (...)

### Searching for Goertler rolls in a gravity flow : some preliminary tests

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 (...)

### Internal wave–boundary layer coupling for a disc oscillating in a density-stratified fluid

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 (...)

### Part 2. Statiscal mechanics of 2D flows

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 (...)

### Statistical Mechanics of 2-D flows

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 (...)

### Part 2. Investigation of the mobile granular layer in bed-load transport

During this seminar I will present the results of of a join experimental, theoretical and numerical investigation of the bed-load layer in laminar shearing flow conditions. For this purpose we (...)

### Part 2. Momentary liquefaction of coastal sands: Field observations and physical modelling

Wave forcing combined to coastline retreat may weaken or unsettle coastal and port structures. Coupling between dynamic flow and seabed mechanical properties at the vicinity of a coastal (...)

### Investigation of the mobile granular layer in bed-load transport

During this seminar I will present the results of of a join experimental, theoretical and numerical investigation of the bed-load layer in laminar shearing flow conditions. For this purpose we (...)

### Momentary liquefaction of coastal sands: Field observations and physical modelling

Wave forcing combined to coastline retreat may weaken or unsettle coastal and port structures. Coupling between dynamic flow and seabed mechanical properties at the vicinity of a coastal (...)

Turbulent vertical eddy diffusivity ($K_z$) and dissipation rate ($\epsilon$) are estimated between 0.5 and 50 m above the sloping side of Great Meteor Seamount, Canary Basin, using 101 moored (...)