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Les séminaires du LMFA ont lieu le vendredi à 11h, et s’adressent à l’ensemble du laboratoire. contact : louis.gostiaux@ec-lyon.fr, wouter.bos@ec-lyon.fr, benjamin.miquel@ec-lyon.fr Pour accéder au (...)
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Les séminaires du LMFA ont lieu le vendredi à 11h, et s’adressent à l’ensemble du laboratoire.
contact : louis.gostiaux@ec-lyon.fr, wouter.bos@ec-lyon.fr, benjamin.miquel@ec-lyon.fr
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Les séminaires du LMFA ont lieu le vendredi à 11h, et s’adressent à l’ensemble du laboratoire. contact : louis.gostiaux@ec-lyon.fr, wouter.bos@ec-lyon.fr, benjamin.miquel@ec-lyon.fr Pour accéder au (...)
Jeudi 15 janvier 2026, 14h, La Doua
A central problem in space and astrophysical plasmas is to understand how a weakly collisional medium is heated by turbulence. In such systems, the cascade is not free to develop in the manner (...)
Mercredi 10 Décembre, 11h, Amphi Seguin, INSA Lyon
Gravity currents are flows caused by a density difference between two fluids, which can be due to temperature and salinity gradients or sediment concentration. Gravity currents can occur in the (...)
Reporté
We investigate the dynamics and dimensional complexity of stratified turbulent flows governed by the Boussinesq equations, combining analytical and data-driven modeling. Stratified turbulence, as (...)
Jeudi 20 Novembre, 11h, ECL (bât. W1, amphi 3)
Lagrangian particles are widely used to investigate dispersion in environmental flows, as they allow for the simultaneous integration of statistics in both space and time, making them (...)
Jeudi 13 Novembre, 11h, ECL (Bat W1, amphi 3)
Turbulent flows are omnipresent in nature and often involve interactions between multiple phases. They range from particle-laden flows with a dispersed phase, such as droplets in atmospheric (...)
Jeudi 30 Octobre, 11h, ECL (Bat W1, amphi 3)
Assessing the impact of human activities on the marine environment is a prerequisite for the authorization of offshore projects (EU directive). It is also a necessary step in the search for (...)
Jeudi 16 Octobre, 11h, ECL (Bat W1, amphi 3)
Decades of observations of the Earth’s equatorial stratosphere reveal a regular oscillation where winds alternate between eastern and western directions. Similar phenomena have also been detected (...)
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