Planet formation at the inner edge of the dead zone II. Outbursts, rings, vortices, and suppression of planetesimal formation
Pith reviewed 2026-06-27 11:30 UTC · model grok-4.3
The pith
Accretion outbursts trigger vortices that suppress planetesimal formation in protoplanetary disks
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
Accretion outbursts are highly unstable to the Rossby-wave instability, with the burst front quickly diffusing into a large number of small-scale vortices that coalesce over time into a single, compact vortex and inducing azimuthal asymmetries. Vortices act as a source of vigorous turbulent diffusion, strongly suppressing planetesimal formation. Our results suggest that azimuthal asymmetries associated with accretion outbursts should be both common and detrimental to planet formation. Nevertheless, planetesimal formation will resume post-burst, as the burst-induced vortices eventually decay and the disk returns to a quiescent state featuring a pressure bump at ~1 au.
What carries the argument
Rossby-wave instability applied to the accretion outburst front in multifluid radiation-hydrodynamical simulations, leading to vortex formation and turbulent diffusion
Load-bearing premise
The two-dimensional vertically integrated simulation setup with growing dust and radiation transport accurately represents the stability and dust behavior in actual three-dimensional disks
What would settle it
Observing an accretion outburst without the formation of vortices or with ongoing planetesimal formation during the burst would contradict the findings
Figures
read the original abstract
Accretion outbursts have been observed in a variety of young stellar objects, but models of their dynamical evolution have been largely limited to axisymmetric models due to their computational cost. We investigate the azimuthal stability of accretion outbursts and the formation of planetesimals during these events. We performed high-resolution 2D, vertically integrated multifluid radiation-hydrodynamical simulations of the inner 10 au of protoplanetary disks with a dynamically growing dust population, including radiation transport and a realistic dust opacity model. Accretion outbursts are highly unstable to the Rossby-wave instability, with the burst front quickly diffusing into a large number of small-scale vortices that coalesce over time into a single, compact vortex and inducing azimuthal asymmetries. Vortices act as a source of vigorous turbulent diffusion, strongly suppressing planetesimal formation. Our results suggest that azimuthal asymmetries associated with accretion outbursts should be both common and detrimental to planet formation. Nevertheless, planetesimal formation will resume post-burst, as the burst-induced vortices eventually decay and the disk returns to a quiescent state featuring a pressure bump at ~1 au.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript uses high-resolution 2D vertically integrated multifluid radiation-hydrodynamical simulations of the inner 10 au of protoplanetary disks with dynamically growing dust and realistic opacity to study accretion outbursts. It claims that outbursts are highly unstable to the Rossby-wave instability, with the burst front diffusing into small-scale vortices that coalesce into a single compact vortex, inducing azimuthal asymmetries; these vortices drive vigorous turbulent diffusion that strongly suppresses planetesimal formation, although formation resumes post-burst once vortices decay and a pressure bump reforms at ~1 au.
Significance. If the central results hold, the work identifies a mechanism linking observed accretion outbursts to common azimuthal asymmetries that hinder planetesimal formation during the burst phase. The multifluid treatment with radiation transport and realistic dust opacity provides a more complete dynamical picture than prior axisymmetric models.
major comments (2)
- [Methods] Methods section (and abstract): The headline claims on RWI-driven vortex formation and strong suppression of planetesimal formation rest exclusively on the 2D vertically integrated equations; no 3D control runs or explicit justification is provided that vertical shear, buoyancy frequency, and dust sedimentation are adequately captured for linear growth rates and nonlinear vortex lifetime, which is load-bearing for the central claim.
- [Results] Results (vortex diffusion and planetesimal suppression): The quantitative assertion that vortices 'strongly suppress' planetesimal formation via turbulent diffusion lacks reported convergence tests, resolution studies, or error analysis on the dust growth implementation, making the strength of the suppression difficult to evaluate independently.
minor comments (1)
- [Abstract] Abstract: The phrase 'high-resolution' is used without stating the grid resolution or cell count, which would improve reproducibility and clarity.
Simulated Author's Rebuttal
We thank the referee for their constructive and detailed comments on our manuscript. We address each major comment point by point below and outline the revisions we will make.
read point-by-point responses
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Referee: [Methods] Methods section (and abstract): The headline claims on RWI-driven vortex formation and strong suppression of planetesimal formation rest exclusively on the 2D vertically integrated equations; no 3D control runs or explicit justification is provided that vertical shear, buoyancy frequency, and dust sedimentation are adequately captured for linear growth rates and nonlinear vortex lifetime, which is load-bearing for the central claim.
Authors: We acknowledge the limitation of using 2D vertically integrated simulations. This dimensionality was chosen to enable the high resolution and extended integration times required to follow vortex coalescence and multifluid dust evolution through the outburst and quiescent phases. Full 3D radiation-hydrodynamical runs with the same physics remain computationally prohibitive. We will revise the Methods section to include an explicit discussion of the 2D approximation, referencing prior work on the validity of vertically integrated models for RWI linear growth and nonlinear vortex evolution, while noting that vertical shear and buoyancy are expected to play a secondary role for the azimuthal dynamics studied here. We will also add a brief discussion of dust sedimentation effects. revision: partial
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Referee: [Results] Results (vortex diffusion and planetesimal suppression): The quantitative assertion that vortices 'strongly suppress' planetesimal formation via turbulent diffusion lacks reported convergence tests, resolution studies, or error analysis on the dust growth implementation, making the strength of the suppression difficult to evaluate independently.
Authors: We agree that convergence and error analysis are needed to support the quantitative strength of the suppression claim. In the revised manuscript we will add a dedicated subsection presenting resolution studies at multiple grid sizes, together with an assessment of numerical convergence in the turbulent diffusion coefficient and its effect on the planetesimal formation threshold. revision: yes
Circularity Check
No circularity: results are direct outputs of described simulations
full rationale
The paper reports outcomes from high-resolution 2D vertically-integrated multifluid radiation-hydrodynamical simulations of disk outbursts. The central claims (RWI instability of the burst front, vortex coalescence, and suppression of planetesimal formation via turbulent diffusion) follow directly from the numerical evolution under the stated equations, opacity model, and initial conditions. No parameter fitting, self-definitional relations, or load-bearing self-citations are present that would make any result equivalent to its inputs by construction. The 2D setup is an explicit modeling choice whose limitations are external to circularity analysis.
Axiom & Free-Parameter Ledger
Reference graph
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