Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability

We conduct 3D hydrodynamic simulations to investigate the nonlinear outcomes and observability of vertical shear instability (VSI) in protoplanetary disks. Our models include both vertically isothermal and thermally stratified disks, with the latter representing realistic conditions featuring a hott...

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Main Authors: Han-Gyeol Yun, Woong-Tae Kim, Jaehan Bae, Cheongho Han
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Astrophysical Journal
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Online Access:https://doi.org/10.3847/1538-4357/ad9f42
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author Han-Gyeol Yun
Woong-Tae Kim
Jaehan Bae
Cheongho Han
author_facet Han-Gyeol Yun
Woong-Tae Kim
Jaehan Bae
Cheongho Han
author_sort Han-Gyeol Yun
collection DOAJ
description We conduct 3D hydrodynamic simulations to investigate the nonlinear outcomes and observability of vertical shear instability (VSI) in protoplanetary disks. Our models include both vertically isothermal and thermally stratified disks, with the latter representing realistic conditions featuring a hotter atmosphere above the midplane. We find that the VSI grows more rapidly and becomes stronger in thermally stratified disks due to enhanced shear, resulting in higher levels of turbulence. At saturation, the turbulence stress reaches α _Rϕ  ≳ 10 ^−3 , more than 1 order of magnitude stronger than the isothermal case. The saturated turbulence is more pronounced near the disk surfaces than at the midplane. On synthetic velocity residual maps, obtained by subtracting the Keplerian rotational velocity, perturbations driven by the VSI manifest as axisymmetric rings in isothermal disks and as ring segments in thermally stratified disks. The latter are visible at disk inclinations as high as 45° in thermally stratified disks. The amplitudes of these residual velocities range from ∼50 to ∼100 m s ^−1 at a 20° inclination, with larger values corresponding to greater thermal stratification. The magnitude of the observed velocity residual increases with the optical depth of the tracer used, as optically thick lines probe the regions near the disk surfaces.
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institution Kabale University
issn 1538-4357
language English
publishDate 2025-01-01
publisher IOP Publishing
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series The Astrophysical Journal
spelling doaj-art-4fe6d02eda7d4044b87aa65766983a562025-01-31T07:41:08ZengIOP PublishingThe Astrophysical Journal1538-43572025-01-0198011510.3847/1538-4357/ad9f42Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and ObservabilityHan-Gyeol Yun0https://orcid.org/0000-0003-4353-294XWoong-Tae Kim1https://orcid.org/0000-0003-4625-229XJaehan Bae2https://orcid.org/0000-0001-7258-770XCheongho Han3https://orcid.org/0000-0002-2641-9964Department of Physics & Astronomy, Seoul National University , Seoul 08826, Republic of Korea ; hangyeol@snu.ac.kr, wkim@astro.snu.ac.kr; SNU Astronomy Research Center, Seoul National University , 1 Gwanak-ro, Gwanak-gu, Seoul 08826, Republic of KoreaDepartment of Physics & Astronomy, Seoul National University , Seoul 08826, Republic of Korea ; hangyeol@snu.ac.kr, wkim@astro.snu.ac.kr; SNU Astronomy Research Center, Seoul National University , 1 Gwanak-ro, Gwanak-gu, Seoul 08826, Republic of KoreaDepartment of Astronomy, University of Florida , Gainesville, FL 32611, USA ; jbae@ufl.eduDepartment of Physics, Chungbuk National University , Cheongju 28644, Republic of Korea ; cheongho@astroph.chungbuk.ac.krWe conduct 3D hydrodynamic simulations to investigate the nonlinear outcomes and observability of vertical shear instability (VSI) in protoplanetary disks. Our models include both vertically isothermal and thermally stratified disks, with the latter representing realistic conditions featuring a hotter atmosphere above the midplane. We find that the VSI grows more rapidly and becomes stronger in thermally stratified disks due to enhanced shear, resulting in higher levels of turbulence. At saturation, the turbulence stress reaches α _Rϕ  ≳ 10 ^−3 , more than 1 order of magnitude stronger than the isothermal case. The saturated turbulence is more pronounced near the disk surfaces than at the midplane. On synthetic velocity residual maps, obtained by subtracting the Keplerian rotational velocity, perturbations driven by the VSI manifest as axisymmetric rings in isothermal disks and as ring segments in thermally stratified disks. The latter are visible at disk inclinations as high as 45° in thermally stratified disks. The amplitudes of these residual velocities range from ∼50 to ∼100 m s ^−1 at a 20° inclination, with larger values corresponding to greater thermal stratification. The magnitude of the observed velocity residual increases with the optical depth of the tracer used, as optically thick lines probe the regions near the disk surfaces.https://doi.org/10.3847/1538-4357/ad9f42Protoplanetary disksHydrodynamicsHydrodynamical simulationsRadiative transferAccretion
spellingShingle Han-Gyeol Yun
Woong-Tae Kim
Jaehan Bae
Cheongho Han
Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
The Astrophysical Journal
Protoplanetary disks
Hydrodynamics
Hydrodynamical simulations
Radiative transfer
Accretion
title Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
title_full Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
title_fullStr Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
title_full_unstemmed Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
title_short Vertical Shear Instability in Thermally Stratified Protoplanetary Disks. II. Hydrodynamic Simulations and Observability
title_sort vertical shear instability in thermally stratified protoplanetary disks ii hydrodynamic simulations and observability
topic Protoplanetary disks
Hydrodynamics
Hydrodynamical simulations
Radiative transfer
Accretion
url https://doi.org/10.3847/1538-4357/ad9f42
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AT jaehanbae verticalshearinstabilityinthermallystratifiedprotoplanetarydisksiihydrodynamicsimulationsandobservability
AT cheonghohan verticalshearinstabilityinthermallystratifiedprotoplanetarydisksiihydrodynamicsimulationsandobservability