Radiative Turbulent Mixing Layers and the Survival of Magellanic Debris
Chad Bustard, Max Gronke

TL;DR
This paper uses high-resolution simulations to show that the Magellanic Stream's Leading Arm and Trailing Stream can survive and even gain mass during infall, challenging classical cloud destruction expectations.
Contribution
It introduces a new analytic framework and simulation results demonstrating cloud survival and mass growth in radiative turbulent mixing layers at high Mach numbers.
Findings
Leading Arm may be composed of high-density cooling clumps.
Mass growth of clouds extends to high Mach number flows.
Hα emission is generally low but can be bright in spots.
Abstract
The Magellanic Stream is sculpted by its infall through the Milky Way's circumgalactic medium, but the rates and directions of mass, momentum, and energy exchange through the Stream-halo interface are relative unknowns critical for determining the origin and fate of the Stream. Complementary to large-scale simulations of LMC-SMC interactions, we apply new insights derived from idealized, high-resolution "cloud-crushing" and radiative turbulent mixing layer simulations to the Leading Arm and Trailing Stream. Contrary to classical expectations of fast cloud breakup, we predict that the Leading Arm and much of the Trailing Stream should be surviving infall and even gaining mass due to strong radiative cooling. Provided a sufficiently supersonic tidal swing-out from the Clouds, the present-day Leading Arm could be a series of high-density clumps in the cooling tail behind the progenitor…
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