{ "id": "1411.7926", "version": "v1", "published": "2014-11-28T16:07:46.000Z", "updated": "2014-11-28T16:07:46.000Z", "title": "Rotation, spectral variability, magnetic geometry and magnetosphere of the Of?p star CPD -28 2561", "authors": [ "G. A. Wade", "R. H. Barbá", "J. Grunhut", "F. Martins", "V. Petit", "J. O. Sundqvist", "R. H. D. Townsend", "N. R. Walborn", "E. Alecian", "E. J. Alfaro", "J. Ma\\' iz Apellániz", "J. I. Arias", "R. Gamen", "N. Morrell", "Y. Nazé", "A. ud-Doula", "the MiMeS Collaboration" ], "comment": "18 pages, accepted by MNRAS", "categories": [ "astro-ph.SR" ], "abstract": "We report magnetic and spectroscopic observations and modeling of the Of?p star CPD -28 2561. Using more than 75 new spectra, we have measured the equivalent width variations and examined the dynamic spectra of photospheric and wind-sensitive spectral lines. A period search results in an unambiguous 73.41 d variability period. High resolution spectropolarimetric data analyzed using Least-Squares Deconvolution yield a Zeeman signature detected in the mean Stokes V profile corresponding to phase 0.5 of the spectral ephemeris. Interpreting the 73.41 d period as the stellar rotational period, we have phased the equivalent widths and inferred longitudinal field measurements. The phased magnetic data exhibit a weak sinusoidal variation, with maximum of about 565 G at phase 0.5, and a minimum of about -335 G at phase 0.0, with extrema approximately in phase with the (double-wave) Halpha equivalent width variation. Modeling of the Halpha equivalent width variation assuming a quasi-3D magnetospheric model produces a unique solution for the ambiguous couplet of inclination and magnetic obliquity angles: (i, beta) or (beta, i)=(35 deg,90 deg). Adopting either geometry, the longitudinal field variation yields a dipole polar intensity Bd=2.6\\pm 0.9~kG, consistent with that obtained from direct modelling of the Stokes V profiles. We derive a wind magnetic confinement parameter eta*\\simeq 100, leading to an Alfv\\'en radius RA\\simeq 3-5~R*, and a Kepler radius RK\\simeq 20~R*. This supports a physical scenario in which the Halpha emission and other line variability have their origin in an oblique, co-rotating 'dynamical magnetosphere' structure resulting from a magnetically channeled wind. Nevertheless, the details of the formation of spectral lines and their variability within this framework remain generally poorly understood.", "revisions": [ { "version": "v1", "updated": "2014-11-28T16:07:46.000Z" } ], "analyses": { "keywords": [ "star cpd", "magnetic geometry", "spectral variability", "halpha equivalent width variation", "resolution spectropolarimetric data" ], "tags": [ "journal article" ], "publication": { "doi": "10.1093/mnras/stu2548", "journal": "Monthly Notices of the Royal Astronomical Society", "year": 2015, "month": "Mar", "volume": 447, "number": 3, "pages": 2551 }, "note": { "typesetting": "TeX", "pages": 18, "language": "en", "license": "arXiv", "status": "editable", "adsabs": "2015MNRAS.447.2551W" } } }