activity
20032026
most citedTurbulent geodynamo simulations: a leap towards Earth's core

275 citations · 1.1k across the 26 of their papers we have counts for

collaborators

26 papers

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…

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-dyn2023★ 4 cited

Dynamic regimes in planetary cores: τ-{\ell} diagrams

Henri-Claude Nataf, Nathanaël Schaeffer

Planetary cores are the seat of rich and complex fluid dynamics, in which the effects of rotation and magnetic field combine. The equilibria governing the strength of the magnetic…

physics.flu-dyn2021★ 20 cited

Mean zonal flows induced by weak mechanical forcings in rotating spheroids

David Cébron, Jérémie Vidal, Nathanaël Schaeffer +2

The generation of mean flows is a long-standing issue in rotating fluids. Motivated by planetary objects, we consider here a rapidly rotating fluid-filled spheroid, which is subjec…

physics.class-ph2020★ 22 cited

The Effects of Robin Boundary Condition on Thermal Convection in a Rotating Spherical Shell

Thibaut Clarté, Nathanaël Schaeffer, Stéphane Labrosse +1

Convection in a spherical shell is widely used to model fluid layers of planets and stars. The choice of thermal boundary conditions in such models is not always straightforward. T…

physics.flu-dyn2019★ 40 cited

Rotating double-diffusive convection in stably stratified planetary cores

Rémy Monville, Jérémie Vidal, David Cébron +1

In planetary fluid cores, the density depends on temperature and chemical composition, which diffuse at very different rates. This leads to various instabilities, bearing the name…