Inertial Modes

Inertial modes are global oscillations of a rotating fluid, restored by the Coriolis force. I’ve studied where they come from and how they show up across very different systems: in a laboratory spherical Couette experiment, where my simulations reproduced modes seen at BTU Cottbus; in the Sun, where eigenmodes computed with the linear code Kore (the same code used to map the onset of convection itself) match recent observations of solar Rossby and HFR vorticity waves; and, more fundamentally, in 3D convection simulations, which show that these modes emerge naturally from rotationally constrained turbulence once the convective Rossby number drops below about one-half - without any external forcing.
Related publications:
- Excitation of Inertial Modes in 3D Simulations of Rotating Convection in Planets and Stars - The Astrophysical Journal (2026)
- Onset of Convection in Rotating Spherical Shells: Variations With Radius Ratio - Earth and Space Science (2023)
- Identification of Inertial Modes in the Solar Convection Zone - The Astrophysical Journal Letters (2022)
- Fluid Dynamics Experiments for Planetary Interiors - Surveys in Geophysics (2022)
- Triadic Resonances in the Wide-Gap Spherical Couette System - Journal of Fluid Mechanics (2018)