Whitworth, Anthony Peter ![]() |
Official URL: http://dx.doi.org/10.1093/mnras/291.3.578
Abstract
Collisions between stable, thermally supported gas clumps produce shock-compressed layers. However, these layers then undergo gravitational fragmentation only if the gas cools — on a dynamical time-scale or faster — to below its pre-shock temperature. Here we present an approximate analytic treatment of post-shock cooling which demonstrates that, under the conditions prevailing in molecular clouds, where the typical collision speeds are ~ 1 km s−1, cooling by dust is likely to be the dominant cooling mechanism, and is sufficiently fast to satisfy this requirement. Cooling by CO appears to be of secondary importance.
Item Type: | Article |
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Date Type: | Publication |
Status: | Published |
Schools: | Physics and Astronomy |
Subjects: | Q Science > QB Astronomy |
Publisher: | Oxford University Press |
ISSN: | 0035-8711 |
Last Modified: | 28 Oct 2022 09:03 |
URI: | https://orca.cardiff.ac.uk/id/eprint/73095 |
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