Interpreting the Mg II h and k Line Profiles of Mira Variables

Astronomy and Astrophysics – Astrophysics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

14 pages, 3 figures; AASTEX v5.0 plus EPSF extensions in mkfig.sty; to appear in ApJ

Scientific paper

10.1086/317131

We use radiative transfer calculations to reproduce the basic appearance of Mg II lines observed from Mira variables. These lines have centroids that are blueshifted by at least 30 km/s from the stellar rest frame. It is unlikely that flow velocities in the stellar atmospheres are this fast, so radiative transfer effects must be responsible for this behavior. Published hydrodynamic models predict the existence of cool, downflowing material above the shocked material responsible for the Mg II emission, and we demonstrate that scattering in this layer can result in Mg II profiles as highly blueshifted as those that are observed. However, our models also show that scattering within the shock plays an equally strong role in shaping the Mg II profiles, and our calculations illustrate the importance of partial redistribution and the effects of being out of ionization equilibrium.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Interpreting the Mg II h and k Line Profiles of Mira Variables does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Interpreting the Mg II h and k Line Profiles of Mira Variables, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Interpreting the Mg II h and k Line Profiles of Mira Variables will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-415284

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.