
Convective wave generation
Convection adjacent to stable stratification generates internal waves.
Daniel Lecoanet
Convection adjacent to stable stratification generates internal waves.
An isolated source of buoyancy can be an effective model for convection.
Convective overshoot and penetration influence convective boundaries.
Geophysical and astrophysical flows can be driven by waves.
Waves traveling in spatial-dependent backgrounds can undergo conversion.
Dedalus is a pseudo-spectral code that can solve nearly arbitrary equations.
Where and how is the solar magnetic field generated?