Magnetohydrodynamic Precipitation

Abstract Circumgalactic gas around massive galaxies and in galaxy-cluster cores generally has a volume-filling component—an atmosphere—with a temperature determined by the potential-well depth of the central galaxy’s halo. If the atmosphere is near hydrostatic equilibrium and is stable to convection, then it can remain nearly homogeneous, as long as it is not too dense. But if its density is great enough, it becomes prone to producing a rain of cold clouds that fall toward the galaxy’s center and accrete onto its central black hole. Here we explain how relatively weak magnetic fields enhance a galactic atmosphere’s tendency to produce cold clouds and how the cold gas becomes organized into vertically elongated, highly magnetized filaments descending at sub-Keplerian speeds. It is intended to complement recent numerical simulations of the process and to serve as a guide to interpreting both simulations and observations of the filamentary gas in hot galactic atmospheres.