2012
DOI: 10.1088/0004-637x/751/2/120
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Modeling the X-Rays Resulting From High-Velocity Clouds

Abstract: With the goal of understanding why X-rays have been reported near some high velocity clouds, we perform detailed 3 dimensional hydrodynamic and magnetohydrodynamic simulations of clouds interacting with environmental gas like that in the Galaxy's thick disk/halo or the Magellanic Stream. We examine 2 scenarios. In the first, clouds travel fast enough to shock-heat warm environmental gas. In this scenario, the X-ray productivity depends strongly on the speed of the cloud and the radiative cooling rate. In order… Show more

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Cited by 11 publications
(19 citation statements)
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“…Similar results were also found in a set of simulations carried out using the FLASH code (Kwak et al 2011;Shelton et al 2012;Gritton et al 2014Gritton et al , 2017, where they studied individual cold clouds interacting with a hot atmosphere. Outflows in these simulations were generally implemented using the constant density and velocity wind-tunnel model.…”
Section: Comparison To Previous Worksupporting
confidence: 78%
“…Similar results were also found in a set of simulations carried out using the FLASH code (Kwak et al 2011;Shelton et al 2012;Gritton et al 2014Gritton et al , 2017, where they studied individual cold clouds interacting with a hot atmosphere. Outflows in these simulations were generally implemented using the constant density and velocity wind-tunnel model.…”
Section: Comparison To Previous Worksupporting
confidence: 78%
“…Note that the speed in the above expression is the speed at which material crosses the shock, which may be somewhat faster than the speed of the cloud, as the shock tends to move away from the cloud as the cloud and shock evolve, at least in the early stages of the cloud's evolution. Hydrodynamical simulations imply that the shock speed exceeds the cloud speed by 10% for strong shocks in cool and warm ambient media induced by initially round clouds (Shelton et al 2012). Note also that, in practice, the average post-shock temperature behind an HVC's bow shock would be lower than that expected from Equation (3) for a number of reasons, especially if the cloud is traveling through relatively dense cool or warm gas: (1) gas toward the side of the cloud will hit the bow shock obliquely, reducing the postshock temperature, (2) the cloud will decelerate as it passes through the dense gas, weakening the shock, and (3) radiative cooling will be important in the dense shocked gas.…”
Section: Strong Shocksmentioning
confidence: 99%
“…We further investigated shock heating using the Case B hydrodynamical models of Shelton et al (2012). In these models, the initially spherical cloud hits warm gas (possibly representing material shed from a preceding cloud; T = 10 4 K, n H = 6.45 × 10 −3 cm −3 ), after passing through hot halo gas (T = 10 6 K, n H = 6.45 × 10 −5 cm −3 ).…”
Section: Predictions From Shelton Et Al (2012) Hvc Modelsmentioning
confidence: 99%
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