Cloud Dispersal in Turbulent Flows

Cold clouds embedded in warm media are very common objects in astrophysics. Their disruption timescale depends strongly on the dynamical configuration. We discuss the evolution of an initially homogeneous cold cloud embedded in warm turbulent gas. Within a couple of dynamical timescales, the filling...

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Main Authors: Heitsch, F, Slyz, A, Devriendt, J, Burkert, A
Format: Journal article
Language:English
Published: 2006
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author Heitsch, F
Slyz, A
Devriendt, J
Burkert, A
author_facet Heitsch, F
Slyz, A
Devriendt, J
Burkert, A
author_sort Heitsch, F
collection OXFORD
description Cold clouds embedded in warm media are very common objects in astrophysics. Their disruption timescale depends strongly on the dynamical configuration. We discuss the evolution of an initially homogeneous cold cloud embedded in warm turbulent gas. Within a couple of dynamical timescales, the filling factor of the cold gas within the original cloud radius drops below 50%. Turbulent diffusivities estimated from the time evolution of radial filling factor profiles are not constant with time. Cold and warm gas are bodily transported by turbulence and mixed. This is only mildly indicated by column density maps. The radiation field within the cloud, however, increases by several orders of magnitudes due to the mixing, with possible consequences for cloud chemistry and evolution within a few dynamical timescales.
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spelling oxford-uuid:2dd56def-153b-4e5e-97ff-9685a65eb83f2022-03-26T12:45:27ZCloud Dispersal in Turbulent FlowsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:2dd56def-153b-4e5e-97ff-9685a65eb83fEnglishSymplectic Elements at Oxford2006Heitsch, FSlyz, ADevriendt, JBurkert, ACold clouds embedded in warm media are very common objects in astrophysics. Their disruption timescale depends strongly on the dynamical configuration. We discuss the evolution of an initially homogeneous cold cloud embedded in warm turbulent gas. Within a couple of dynamical timescales, the filling factor of the cold gas within the original cloud radius drops below 50%. Turbulent diffusivities estimated from the time evolution of radial filling factor profiles are not constant with time. Cold and warm gas are bodily transported by turbulence and mixed. This is only mildly indicated by column density maps. The radiation field within the cloud, however, increases by several orders of magnitudes due to the mixing, with possible consequences for cloud chemistry and evolution within a few dynamical timescales.
spellingShingle Heitsch, F
Slyz, A
Devriendt, J
Burkert, A
Cloud Dispersal in Turbulent Flows
title Cloud Dispersal in Turbulent Flows
title_full Cloud Dispersal in Turbulent Flows
title_fullStr Cloud Dispersal in Turbulent Flows
title_full_unstemmed Cloud Dispersal in Turbulent Flows
title_short Cloud Dispersal in Turbulent Flows
title_sort cloud dispersal in turbulent flows
work_keys_str_mv AT heitschf clouddispersalinturbulentflows
AT slyza clouddispersalinturbulentflows
AT devriendtj clouddispersalinturbulentflows
AT burkerta clouddispersalinturbulentflows