The magnetic field of Betelgeuse: a local dynamo from giant convection cells? (original) (raw)

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Abstract

Context. Betelgeuse is an M supergiant with a complex and extended atmosphere, which also harbors spots and giant granules at its surface. A possible magnetic field could contribute to the mass loss and to the heating of the outer atmosphere.
Aims: We observed Betelgeuse, to directly study and infer the nature of its magnetic field.
Methods: We used the new-generation spectropolarimeter NARVAL and the least square deconvolution (LSD) method to detect circular polarization within the photospheric absorption lines of Betelgeuse.
Results: We have unambiguously detected a weak Stokes V signal in the spectral lines of Betelgeuse, and measured the related surface-averaged longitudinal magnetic field B_ℓ at 6 different epochs over one month. The detected longitudinal field is about one Gauss and is apparently increasing on the time scale of our observations.
Conclusions: This work presents the first direct detection of the magnetic field of Betelgeuse. This magnetic field may be associated to the giant convection cells that could enable a “local dynamo”.

Based on observations obtained at the Télescope Bernard Lyot (TBL) at Observatoire du Pic du Midi, CNRS/INSU and Université de Toulouse, France.

Publication:

Astronomy and Astrophysics

Pub Date:

June 2010

DOI:

10.1051/0004-6361/201014925

10.48550/arXiv.1005.4845

arXiv:

arXiv:1005.4845

Bibcode:

2010A&A...516L...2A

Keywords:

E-Print:

Accepted as a letter for A&amp