collaborators

6 papers

physics.flu-dyn2026

Magnetohydrodynamic drag on an oscillating sphere in a rotating spherical cavity

David Cébron, Paolo Personnettaz

The drag on an oscillating sphere is a classical fluid-mechanics problem, yet no existing theory simultaneously accounts for confinement, rotation, viscosity and magnetic fields. W…

physics.flu-dyn2026

Semi-convection in rotating spherical shells: flows, layers and dynamos

Paul Pružina, Nathanaël Schaeffer, David Cébron

Large regions of giant planets are thought to possess unstable thermal gradients stabilised by gradients in heavy-element composition. The fluid can then develop semi-convection, a…

physics.geo-ph2026

Ohmic and viscous damping of inner core translational oscillations

Paolo Personnettaz, David Cébron, Nathanaël Schaeffer +2

Large earthquakes can trigger translational oscillations of Earth's inner core (Slichter modes), yet their damping remains uncertain. Using simulations, we quantify viscous and Ohm…

physics.geo-ph2026

Did lunar tides sustain the early Earth's dynamo?

Jérémie Vidal, David Cébron

Geological data show that, early in its history, the Earth had a large-scale magnetic field with an amplitude comparable to the one of the present geomagnetic field. However, its o…

astro-ph.EP2025

Planetary dynamos driven by semiconvection in stably stratified layers

Paul Pružina, David Cébron, Nathanaël Schaeffer

Stably stratified fluid layers are common in gaseous planets, stellar interiors, and planetary cores, and have long been considered incapable of sustaining dynamo action. Here, we…

physics.flu-dyn2025

Geophysical flows over topography, a playground for laboratory experiments

Jérémie Vidal, Jérôme Noir, David Cébron +4

Physicists face major challenges in modelling multi-scale phenomena that are observed in geophysical flows (e.g. in the Earth's oceans and atmosphere, or liquid planetary cores). I…