The complex inner disk of the Herbig Ae star HD 100453 with VLTI/MATISSE
Pith reviewed 2026-05-17 05:41 UTC · model grok-4.3
The pith
MATISSE data confirm the inner disk of HD 100453 is misaligned with the outer disk at 47.5 degrees inclination and 0.27 au radius.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
The parametric model fitted to the combined PIONIER, GRAVITY, and MATISSE observations finds an inclination of approximately 47.5 degrees and a position angle of 83.6 degrees for the inner disk, which supports a strong misalignment with the outer disk. From the symmetric temperature gradient the inner disk radius is derived as roughly 0.27 au, with dust surface densities of about 10 to the minus 3.2 grams per square centimeter and vertical optical depths of 0.1 to 0.06 at the sublimation edge. Same-night MATISSE and GRAVITY measurements indicate that higher-order asymmetries are needed to explain the interferometric signals, a conclusion reinforced by MATISSE snapshot image reconstruction.
What carries the argument
The symmetric temperature gradient parametric model fitted jointly to multi-wavelength interferometric visibilities and closure phases, together with snapshot image reconstruction.
If this is right
- The quantified misalignment angles provide direct constraints on the dynamical history of the inner and outer disk.
- Higher-order asymmetries must be included in models to match the observed signals at L and K bands.
- Coordinated GRAVITY and MATISSE observations are required to test whether the asymmetries persist or evolve.
- The derived inner radius and optical depth values limit the possible dust composition and distribution near the star.
Where Pith is reading between the lines
- If the asymmetries trace disk instabilities, they may alter the pathways and timescales for planet migration and growth.
- Future observations spaced months apart could test whether the higher-order features vary on orbital timescales.
- The same joint modeling approach could be applied to other Herbig stars known to host misaligned disks to check for common patterns.
Load-bearing premise
That a single symmetric temperature gradient remains valid across the full wavelength range and that the disk structure shows no significant evolution between observations taken years apart.
What would settle it
New multi-wavelength interferometric data that cannot be reproduced by the symmetric temperature gradient model, or repeated observations that reveal clear structural changes on timescales shorter than four years.
Figures
read the original abstract
The inner regions of planet-forming disks hold invaluable insights for our understanding of planet formation. The disk around the Herbig star HD 100453 presents one such environment, with an inner disk that is significantly misaligned with respect to the outer disk. This paper expands the existing H-band (PIONIER) and K-band (GRAVITY) interferometric studies of the HD 100453 inner disk to the L-band with the MATISSE VLTI instrument. With snapshot data spanning approximately four years we aim for a more comprehensive understanding of the inner disk structures and their potential time evolution. Based on the MATISSE data obtained, we use a combination of analytical models and image reconstruction to constrain the disk structure. Additionally, we fit a temperature gradient model to the selected wavelength range of PIONIER, GRAVITY and MATISSE to derive physical properties of the inner regions. Our parametric model finds an inclination of $\sim 47.5^\circ$ and a position angle of $\sim 83.6^\circ$, which corroborates the case of strong inner-outer disk misalignment. From the symmetric temperature gradient we derive an inner disk radius around $\sim0.27$ au, with dust surface densities of $\Sigma_{\rm{subl}} \approx 10^{-3.2}$ g/cm$^2$ and vertical optical depth $\tau_{\rm{z, subl}} \approx 0.1-0.06$. Same-night MATISSE and GRAVITY observations indicate the necessity for higher-order asymmetries to explain the interferometric signals, which is further supported by a MATISSE snapshot image reconstruction. The chromatic interferometric data reveal the likely need for higher-order asymmetries to explain the inner disk of HD~100453, suggesting a possible origin in dynamic interactions or disk instabilities. Coordinated multi-wavelength infrared interferometric observations with GRAVITY and MATISSE will be crucial to confirm these findings and uncover its underlying nature.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper presents new L-band VLTI/MATISSE interferometric snapshot observations of the inner disk of the Herbig Ae star HD 100453, extending prior H-band (PIONIER) and K-band (GRAVITY) studies. It combines parametric modeling assuming a symmetric temperature gradient with image reconstruction on multi-epoch data spanning ~4 years to derive an inner-disk inclination of ~47.5°, position angle of ~83.6°, sublimation radius of ~0.27 au, dust surface density Σ_subl ≈ 10^{-3.2} g cm^{-2}, and vertical optical depth τ_z,subl ≈ 0.1-0.06. The authors conclude that same-night MATISSE+GRAVITY data and the MATISSE image reconstruction require higher-order asymmetries, pointing to possible dynamic interactions or instabilities.
Significance. If the results hold, the work supplies quantitative multi-wavelength constraints on a strongly misaligned inner disk, a key laboratory for planet formation and disk dynamics. Strengths include the joint use of parametric fits and image reconstruction plus same-night multi-instrument coverage; these provide direct, falsifiable measurements of misalignment and inner radius that can be tested against hydrodynamic models of warped disks.
major comments (2)
- [Parametric modeling / temperature gradient fit] Parametric modeling section (temperature-gradient fit to combined PIONIER/GRAVITY/MATISSE visibilities): the headline inner radius (~0.27 au), Σ_subl, and τ_z,subl are derived under the assumption of azimuthal symmetry in the temperature profile, yet the manuscript states that same-night MATISSE+GRAVITY data plus the MATISSE snapshot reconstruction both require higher-order asymmetries. If non-axisymmetric brightness variations are present at L-band wavelengths that dominate the sublimation-radius constraint, the azimuthally averaged model will bias the inferred sublimation front location and vertical optical depth.
- [Data combination and multi-epoch discussion] Multi-epoch analysis: the paper combines snapshot observations spanning four years without explicit tests for time variability or evolution. Any low-level changes in disk structure between epochs would decouple the wavelength regimes and undermine the asymmetry interpretation drawn from the combined dataset.
minor comments (2)
- [Abstract] Abstract: reported values for inclination, position angle, and inner radius lack explicit uncertainties or model-selection details; adding these would improve clarity.
- [Parametric model description] Notation: the precise definition and wavelength dependence of the vertical optical depth τ_z,subl should be stated explicitly when introduced in the temperature-gradient model.
Simulated Author's Rebuttal
We thank the referee for their careful reading of the manuscript and for the constructive comments. We address each major comment below and describe the changes incorporated in the revised version.
read point-by-point responses
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Referee: [Parametric modeling / temperature gradient fit] Parametric modeling section (temperature-gradient fit to combined PIONIER/GRAVITY/MATISSE visibilities): the headline inner radius (~0.27 au), Σ_subl, and τ_z,subl are derived under the assumption of azimuthal symmetry in the temperature profile, yet the manuscript states that same-night MATISSE+GRAVITY data plus the MATISSE snapshot reconstruction both require higher-order asymmetries. If non-axisymmetric brightness variations are present at L-band wavelengths that dominate the sublimation-radius constraint, the azimuthally averaged model will bias the inferred sublimation front location and vertical optical depth.
Authors: We agree that the parametric temperature-gradient model assumes azimuthal symmetry and that detected higher-order asymmetries could in principle introduce a bias in the derived average parameters, particularly since the L-band data contribute strongly to the sublimation-radius constraint. The symmetric model was adopted to obtain a first-order, azimuthally averaged description that can be compared directly with earlier H- and K-band results. In the revised manuscript we have added an explicit discussion of this limitation in the modeling section, clarifying that the reported inner radius, surface density and optical depth represent effective azimuthally averaged quantities and noting the complementary role of the image reconstruction in revealing asymmetries. revision: yes
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Referee: [Data combination and multi-epoch discussion] Multi-epoch analysis: the paper combines snapshot observations spanning four years without explicit tests for time variability or evolution. Any low-level changes in disk structure between epochs would decouple the wavelength regimes and undermine the asymmetry interpretation drawn from the combined dataset.
Authors: The observations consist of snapshots acquired over approximately four years. We verified that the visibility data from the different epochs are consistent within the measurement uncertainties before combining them. In the revised manuscript we have added a short paragraph in the observations and data-reduction section that documents this consistency check and states the assumption of temporal stability over the observed baseline. We acknowledge that the current dataset does not permit a detailed variability analysis and that more densely sampled observations would be required to fully exclude low-level structural evolution. revision: yes
Circularity Check
No significant circularity; parameters derived from direct fitting to new interferometric data
full rationale
The paper fits a symmetric temperature gradient model to combined PIONIER/GRAVITY/MATISSE visibilities and closure phases to derive inclination (~47.5°), position angle (~83.6°), inner radius (~0.27 au), surface density, and optical depth. These are outputs of a standard parametric fit to external observational constraints rather than any reduction by construction to prior fitted quantities or self-citations. The acknowledgment of higher-order asymmetries from same-night data and image reconstruction is presented as an independent finding, not a loop that forces the symmetric-model results. No self-definitional steps, fitted inputs renamed as predictions, or load-bearing self-citations appear in the derivation chain. The work is self-contained against the new VLTI data.
Axiom & Free-Parameter Ledger
free parameters (5)
- inclination =
~47.5°
- position angle =
~83.6°
- inner disk radius =
~0.27 au
- dust surface density at sublimation =
~10^{-3.2} g/cm²
- vertical optical depth at sublimation =
0.1-0.06
axioms (2)
- domain assumption Inner disk can be described by a symmetric temperature gradient model that applies uniformly from H to L band
- domain assumption Interferometric signals are adequately captured by a combination of analytical parametric models and snapshot image reconstruction
Reference graph
Works this paper leans on
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[1]
Astropy Collaboration, Price-Whelan, A. M., Lim, P. L., et al. 2022, ApJ, 935, 167 Ataiee, S., Pinilla, P., Zsom, A., et al. 2013, A&A, 553, L3 Avenhaus, H., Quanz, S. P., Schmid, H. M., et al. 2017, AJ, 154, 33 Bae, J., Isella, A., Zhu, Z., et al. 2023, in Astronomical Society of the Pacific Conference Series, V ol. 534, Protostars and Planets VII, ed. S...
work page 2022
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[2]
Typically IR interferometry reports the error estimate on fitted parameters as the 16%−84% intervals from settled MCMC chains. An important underlying assump- tion is that this assumes the measurement errors are independent and Gaussian distributed. However, this method is flawed as in- terferometric observables, especially when working with multi- ple sp...
work page 2020
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[3]
(g/cm2) = 3.208+0.001 0.001 0.280 0.284 0.288 0.292 Apio (Jy) Apio (Jy) = 0.285+0.002 0.002 3.50 3.25 3.00 2.75 ppio ppio = 3.149+0.133 0.137 0.4876 0.4882 0.4888 0.4894 Agrav (Jy) Agrav (Jy) = 0.488+0.000 0.000 3.040 3.032 3.024 3.016 pgrav pgrav = 3.025+0.005 0.005 0.692 0.696 0.700 0.704 0.708 Amat (Jy) Amat (Jy) = 0.700+0.002 0.002 0.2710 0.2713 0.271...
work page 2095
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[4]
(g/cm2) 0.280 0.284 0.288 0.292 Apio (Jy) 3.50 3.25 3.00 2.75 ppio 0.4876 0.4882 0.4888 0.4894 Agrav (Jy) 3.040 3.032 3.024 3.016 pgrav 0.692 0.696 0.700 0.704 0.708 Amat (Jy) 0.0 0.2 0.4 0.6 pmat pmat = 0.432+0.087 0.088 Fig. D.1.Temperature gradient model best-fit MCMC chains, forR out =10 AU, after removing burn-in to the combined PIONIER, GRA VITY & M...
work page 2000
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[5]
Appendix E: MATISSE/GRAVITY comparison of closure phases on the same nights Figure E.1 shows a comparison of how the simulated closure phases for the skewed ring look in practice. From both visual inspection and theχ 2 r -maps it is clear that theθ skwPA ∼92 ◦ rep- resents the MATISSE data much better than the best fit value θskwPA ∼ −173 ◦ from the GRA V...
work page 2021
discussion (0)
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