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Hydrodynamical models of clumping beyond 50 R∗

We present one-dimensional, time-dependent models of the clumps generated by the linedeshadowing instability. In order to follow the clumps out to distances of more than 1000 R∗, we use an efficient moving-box technique. We show that, within the approximations, the wind can remain clumped well into the formation region of the radio continuum.

Identiferoai:union.ndltd.org:Potsdam/oai:kobv.de-opus-ubp:1803
Date January 2007
CreatorsRunacres, M. C.
PublisherUniversität Potsdam, Extern. Extern
Source SetsPotsdam University
LanguageEnglish
Detected LanguageEnglish
TypeInProceedings
Formatapplication/pdf
Rightshttp://opus.kobv.de/ubp/doku/urheberrecht.php

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