VARYING WINDS = INSTABILITIES
One of the interesting features of these models is the presence
of hydrodynamic instabilities. These include...
- KH: Kelvin-Helmholtz
- This shearing instability has already been seen in many of the
previous simulations, particularly when the asymmetry of the flow
directs the hot bubble along the inside surface of the shell.
- RT: Rayleigh-Taylor
- If the momentum in the fast wind is gradually increasing, the
shell will be accelerated, leading to an RT instability of the thin shell.
- PDTSO: Pressure-Driven Thin-Shell Overstability
- If a thin shell is formed via radiative cooling, and if the momentum
of the wind decreases leading to a deceleration of this thin shell, the
PDTSO first described by Vishniac will ripple the shell.
- NTSI: Nonlinear Thin-Shell Instability
- If both the leading and reverse wind shocks are strongly radiative,
leading to a thin shell bounded on both sides by narrow radiative shocks,
the shell is wildly unstable to the NTSI.