Supernovae drive large-scale, incompressible turbulence through small-scale instabilities
James R. Beattie
TL;DR
This work identifies the unstable contact discontinuity in SNR cooling layers as the primary driver of incompressible turbulence in SN-driven galactic environments. By analyzing ~100 localized SNRs from high-resolution simulations, it derives a direct link between baroclinicity and the incompressible velocity field, establishing a predictive relation between baroclinic enstrophy and the velocity spectrum. The unstable layer exhibits a $k^{3/2}$ baroclinic spectrum and produces local incompressible modes with $\\\mathcal{P}_{\\bm{u}_s}(k) \\\propto k^{-3/2}$, while the shell's surface modes follow a 2D turbulence scaling $C(\\ell) \\\propto \\\ell^{-8/3}$. The study further shows that young SNRs can shed these surface modes into the surrounding ISM when a vortex-stretching timescale allows, linking small-scale instabilities to the large-scale turbulence cascade and providing a mechanism for SN-driven turbulence to influence kiloparsec-scale dynamics. The results offer a new phenomenology for turbulence in galaxies and highlight the role of Vishniac-like shell instabilities in seeding large-scale, incompressible turbulence through an inverse cascade.
Abstract
The sources of turbulence in our Galaxy may be diverse, but core-collapse supernovae (SNe) alone provide enough energy to sustain a steady-state galactic turbulence cascade at the observed velocity dispersion. By localizing and analyzing supernova remnants (SNRs) in high-resolution SN-driven galactic disk cut-out simulations from Beattie et al. (2025), I show that isolated SNRs source incompressible turbulence through baroclinic vorticity generation localized at the unstable contact discontinuity. Through the spherical harmonic power spectrum of the corrugations, I provide evidence that this process is seeded by surface instabilities and 2D turbulence on the shell, which corrugates and folds the interface, becoming the strongest source of baroclinicity in the simulations. I present an analytical relation for a baroclinicity-fed incompressible mode (co)spectrum, which matches that observed in the simulated SNRs, and reveals a $k^{-17/20}$ spectrum that drives the turbulence. I show that vortex stretching allows for modes to be shed from the contact discontinuity into the surrounding medium and derive a timescale criteria for this process, revealing that young SNR with radii close to the cooling radius are efficient at radiating turbulence. The unstable layer produces a spectrum of incompressible modes $\propto k^{-3/2}$ locally within the SNRs. Through the inverse cascade mechanism revealed in Beattie et al. (2025), this opens the possibility that the $k^{-3/2}$ spectrum, arising from corrugated folds in the unstable layer, imprints itself on kiloparsec scales, thereby connecting small-scale structure in the layer to the large-scale incompressible turbulence cascade.
