Laboratoire des Écoulements Géophysiques et Industriels




Supervisory authorities

CNRS

Our partners

Search


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

Group seminars

Informal seminars (20 min of presentation, usually Thursday at 1 pm) are organized in the team.

Send an email to:
Rémi Chassagne  .

Next seminars:

- 2023/11/09 Thursday 1pm - Thibault Leduque -

List of all seminars:

Page(s) : < | 1 | ... | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 |

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 (...)

Read more

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 (...)

Read more

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 (...)

Read more

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 (...)

Read more

Internal waves measurements above Great Meteor seamount : turbulence and mixing

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 (...)

Read more

Second harmonic behavior in the 2D internal wave reflection problem.

The generation of the second harmonic wave is studied through a weakly non linear inviscid theory based on Thorpe (1987) and extended to finite width plane waves. It turns out that, contrary to (...)

Read more

Ekman boundary layer - a local stability analysis

The Ekman boundary layer describes fluid flow near a solid boundary in the presence of background rotation. Ekman dynamics plays a critical role in the understanding of several atmospheric and (...)

Read more

Development and Implementation of a Wall Model for the Immersed Boundary Method

Florian Mintgen est en visite au LEGI/ERES dans le cadre
d’un stage Master-Honour (3 mois) de l’université de Munich.
Il a présenté vendredi 18 décembre 2009 les résultats de son projet
de Master effectué sous la direction de M. Manhart (TUM) sur le sujet suivant:

Read more

Destabilizing a seiche with an movable dam.

Volcanic tremors are seismic signals emanating from uid channels encased in rock. The understanding of the mechanism of this phenomenon is of great importance to improve evaluation of volcanic (...)

Read more

Quantum vortices in a glass of Bose-Einstein condensate

Bose-Einstein condensation occurs for bosons when, for a temperature low enough (typically a few nanokelvins for a gaseous condensate), a macroscopic fraction of the bosons gathers in the quantum (...)

Read more

Page(s) : < | 1 | ... | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 |