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Accueil > Équipes > Équipe MEIGE > Diffusion scientifique > Séminaires internes

Séminaires internes

Des séminaires internes informels (20 min de présentation, habituellement jeudi à 13h) sont régulièrement organisés dans l’équipe.

Pour des infos ou demandes, envoyer un courriel à  : Rémi Chassagne  .

Prochains séminaires :

- 2023/01/09 Jeudi 13h00 - Thibault Leduque -

La liste plus complète des séminaires à venir et passés :

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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 (...)

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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 (...)

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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 (...)

Lire la suite

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 (...)

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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 (...)

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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 (...)

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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 (...)

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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 :

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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 (...)

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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 (...)

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