Linear polarization of rapidly rotating ultracool dwarfs

TL;DR

This study investigates near-infrared linear polarization in rapidly rotating ultracool dwarfs, revealing a significant fraction exhibit measurable polarization likely due to dusty atmospheres and oblate shapes, with variability indicating atmospheric weather patterns.

Contribution

First systematic polarimetric survey of ultracool dwarfs linking polarization to rotation and atmospheric phenomena, highlighting long-term variability and potential atmospheric weather effects.

Findings

Approximately 40% of the sample shows linear polarization.

Higher polarization fractions are associated with the fastest rotators.

Long-term variability suggests atmospheric weather phenomena.

Abstract

Aims. We aim at studying the near infrared linear polarization signal of rapidly rotating ultracool dwarfs with spectral types ranging from M7 through T2 and projected rotational velocities vsini >= 30 km s^{-1}. All these dwarfs are believed to have dusty atmospheres and oblate shapes, an appropriate scenario to produce measurable linear polarization of the continuum light.\\ Methods. Linear polarimetric images were collected in the J-band for a sample of 18 fast-rotating ultracool dwarfs, five of which were also observed in the Z-band using the LIRIS spectrograph on the Cassegrain focus of the 4.2-m William Herschel Telescope. The measured median uncertainty in the linear polarization degree is +/-0.13% for our sample, which allowed us to detect polarization signatures above ~0.39% with a confidence of >=3\sigma.\\ Results. About 40+/-15% of the sample is linearly polarized in the Z- and J-bands. All positive detections have linear polarization degrees ranging from 0.4% to 0.8% in both filters independently of spectral type and spectroscopic rotational velocity. However, simple statistics point at the fastest rotators (vsini >=60 km s^{-1}) having a larger fraction of positive detections and a larger averaged linear polarization degree than the moderately rotating dwarfs (vsini=30--60 km s^{-1}). Our data suggest little linear polarimetric variability on short time scales (i.e., observations separated by a few ten rotation periods), and significant variability on long time scales (i.e., hundred to thousand rotation cycles), supporting the presence of "long-term weather" in ultracool dwarf atmospheres.