2020
DOI: 10.1093/mnrasl/slaa033
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Is multiphase gas cloudy or misty?

Abstract: Cold T ∼ 10 4 K gas morphology could span a spectrum ranging from large discrete clouds to a fine 'mist' in a hot medium. This has myriad implications, including dynamics and survival, radiative transfer, and resolution requirements for cosmological simulations. Here, we use 3D hydrodynamic simulations to study the pressure-driven fragmentation of cooling gas. This is a complex, multi-stage process, with an initial Rayleigh-Taylor unstable contraction phase which seeds perturbations, followed by a rapid, viole… Show more

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Cited by 80 publications
(73 citation statements)
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“…Using this model, a cold cloud in typical CGM conditions can have a characteristic size somewhere in the range of ℓ 1 pc 1 kpc cloudlet , depending on the gas pressure, metallicity, and UV background radiation. Additionally, depending on the conditions of the surrounding medium, the true size of cold gas clouds may be significantly larger, as clouds can coagulate to form larger structures (Gronke & Oh 2020).…”
Section: Cold Cloud Sizesmentioning
confidence: 99%
“…Using this model, a cold cloud in typical CGM conditions can have a characteristic size somewhere in the range of ℓ 1 pc 1 kpc cloudlet , depending on the gas pressure, metallicity, and UV background radiation. Additionally, depending on the conditions of the surrounding medium, the true size of cold gas clouds may be significantly larger, as clouds can coagulate to form larger structures (Gronke & Oh 2020).…”
Section: Cold Cloud Sizesmentioning
confidence: 99%
“…They indicate two processes for which the condensation is shredded apart through high vorticity, and they are thus explained differently from the 'shattering' mechanism of McCourt et al (2018). In the first process, vorticity is generated in a rapid expansion phase by a Richtmyer-Meshkov (Richtmyer 1960;Meshkov 1972) process before the condensation fragments into smaller pieces (Gronke & Oh 2020). In the second process, smaller condensations are fragmented by pressure gradients between merging large clouds (Waters & Proga 2019a).…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…There is no consensus about the mechanism for fragmentation of high beta hydrodynamic gas clouds (see e.g. Waters & Proga 2019a,b;Gronke & Oh 2020;Jennings & Li 2021;Das et al 2021). One of those processes is 'shattering' (McCourt et al 2018), where a cloud fragments into small pieces that each cool isobarically, independently of each other.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…• Multiple clouds; Kinematic Structure. To account for the observations, a line of sight has to pass through ∼ 100 − 1000 mixing layers; which is conceivable if the cold gas has a 'fog-like' structure (McCourt et al 2018;Gronke & Oh 2020b). Cold gas in a turbulent medium acquires a wide-ranging, almost scale-free range of sizes, but the covering fraction is dominated by small cloudlets (Gronke et al 2021, in preparation).…”
Section: Discussionmentioning
confidence: 99%