1995
DOI: 10.1007/bf00627346
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Low velocity shock-cloud encounters I.

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“…In the latter case the vorticity is generated in a sheet at the model cloud surface, and this material is swept behind the cloud by the shock, resulting in comet-shaped clouds (or filaments with "heads"). Such structures are found even in simulations of low-velocity shock-cloud interactions (Horvath & Toth 1995).…”
Section: Comparison Of Induced Velocity Amplitudes With Observationsmentioning
confidence: 97%
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“…In the latter case the vorticity is generated in a sheet at the model cloud surface, and this material is swept behind the cloud by the shock, resulting in comet-shaped clouds (or filaments with "heads"). Such structures are found even in simulations of low-velocity shock-cloud interactions (Horvath & Toth 1995).…”
Section: Comparison Of Induced Velocity Amplitudes With Observationsmentioning
confidence: 97%
“…Vanhala & Cameron (1998) presented three dimensional simulations, including a very detailed treatment of the cooling rates, that addressed the question of disruption versus gravitational instability, for relatively high shock speeds and relatively sharp-edged (Gaussian) clouds. Horvath & Toth (1995) presented two-dimensinal simulations of lower-velocity non-disruptive shock-cloud interactions. In all these simulations, at least for early times, the vorticity is present only as a sheet on the outside of the cloud.…”
Section: Previous Workmentioning
confidence: 99%