arXiv subjects

Yu-Ru Chou

Publications and source records attributed to Yu-Ru Chou.

3 recordsLinked to original sources

arXiv2026

PRODIGE -- envelope to disk with NOEMA VIII. Sulfur oxides trace a shock caused by a streamer in the inner envelope of a protostar

(Abridged) Recently, streamers have been observed causing shocks at the outer edge of protoplanetary disks. The study of sulfur-bearing species can help us to understand the physical and chemical changes caused by infalling streamers toward their landing positions. We study the physical properties traced by SO$_2$ and SO toward the Class I protostar Per-emb 50, which is possibly related to the streamer infalling toward its disk. We present new NOEMA A-array observations as part of the large program "Protostars and Disks: Global Evolution" (PRODIGE). We analyzed the morphology of SO$_2$ and SO, and complement our interpretations with additional H_$2$CO and CO data from the same program. We compared the SO$_2$ and SO morphology with an infalling-rotating model. We applied Bayesian model selection to the brightest SO$_2$ line to disentangle the different kinematic components traced by this molecule. We used Local Thermodynamic Equilibrium (LTE) and non-LTE analyses to determine the temperature and density of the SO$_2$ emission. There are two separate peaks of SO$_2$ emission offset toward the southwest of Per-emb 50, one brighter (peak 1) at about 180 au from the protostar, and a weaker one (peak 2) at about 400 au. Peak 2 is blueshifted with respect to an infalling-rotating envelope. We propose that this peak is caused by the shock between the inner envelope and the streamer. Peak 1 is consistent with the expected envelope motion, and could thus be caused by shocks at the disk-envelope interface, but potential streamer influence cannot be neglected. Both peaks show abundance ratios consistent with a low velocity shock ($\sim 3-4$ \kms) when compared with shock models. Streamers can affect the physical and chemical structure of both disks and envelopes, suggesting that streamers can play an important role in shaping both structures in the embedded stages of star formation.

astro-ph.SR↗

arXiv2025

Variability of the DG Tau Forbidden Emission Line Low Velocity Component

Optical Forbidden Emission Lines (FELs) come from transitions with long radiative decay times needing low density gas where collisions between atoms are rare. They are produced in the outflows driven by young stellar objects. These lines trace distinct velocity components, including a Low Velocity Component (LVC), which may be tracing a magneto hydrodynamic (MHD) or photoevaporative (PE) wind. We study the jet and LVC of the star DG Tau, whose jet velocity has decreased since 2006. We aim to investigate a link between the high velocity jet and the LVC and clarify the LVC origin as an MHD or PE wind by studying spectral \& spatial changes over time. Using kinematic fitting \& spectro-astrometry, we analyse three epochs of spectra spanning ~18 years. A ~100 km/s decrease in velocity from 2003 to 2021 aligns with known slowing of the jet. Fitting of the [O I] {\lambda}6300, [O I] {\lambda}5577, and [S II] {\lambda}6731 lines reveal complex FEL profiles, with up to six blue-shifted components and a redshifted wing, in agreement with Chou et al. (2025). We see three LVC sub-components (LVC-H, LVC-M, and LVC-L) that are consistent with entrained jet material, disk wind, and dense upper disk atmosphere respectively. While jet components vary in time, the LVC remains quite stable, with changes in the relative brightness of each sub-component. The results cannot distinguish between a MHD or PE wind origin for the LVC. A limit of less than 2 au is put on the de projected height of the LVC-M in [O I] {\lambda}5577, where there is no jet contribution. This supports a disk wind and may favor an MHD wind origin. The near constant peak velocity of LVC-M needs further study in context of a shared origin for jets and MHD winds. Future work needs observations with higher spectral resolution and time cadence to resolve blended components and examine a possible time lag between changes in the jet and LVC.

astro-ph.SR↗

arXiv2025

A Spectroastrometric Study of the Low-velocity Wind from DG Tau A

We obtained high spectral resolution spectra ($\Delta v$ $\sim$ 2.5 km s$^{-1}$) for DG Tau A from 4800 \r{A} to 7500 \r{A} using Subaru High Dispersion Spectrograph (HDS) for the first time. The low-velocity components (LVCs, |$v$| < 100 km s$^{-1}$) were observed in the [O I] 5577, 6300, 6364 \r{A}, [S II] 6716, 6731 \r{A} lines. The offset position spectra observed in the LVCs show a "negative velocity gradient", supporting the presence of a wide-angled wind associated with the LVC emission. The offset position spectra observed in a component within the LVC velocity range between -16 km s$^{-1}$ to -41 km s$^{-1}$, namely, LVC-M, show a "negative velocity gradient'', supporting the presence of a wide-angled wind. With 12-70 au wind lengths measured using spectroastrometry, we estimate a lower limit to the wind mass-loss rate of $\sim$10$^{-8}$ M$_\odot$ yr$^{-1}$. In addition to the LVCs, we identify two high-velocity components (HVCs, |$v$| > 100 km s$^{-1}$) associated with the collimated jet in 26 lines ([N I], [N II], [O I], [O II], [O III], [S II], [Ca II], [Fe II], H$\alpha$, H$\beta$, He I). The one with a clear spatial offset from the star ($n_e$ $\sim$10$^4$ cm$^{-3}$, HVC1) is associated with an internal shock surface of the jet, while the other at the base ($n_e$ $\sim$10$^6$ cm$^{-3}$, HVC2) may be a stationary shock component. We find that the observed line profiles and the spatial scales of the LVC emission do not agree with the existing predictions for photoevaporative or magnetohydrodynamical (MHD) disk winds. These could be explained by the X-wind model, but synthetic observations are required for detailed comparisons.

astro-ph.SR↗