Upward Overshooting in Turbulent Compressible Convection. III. Calibrate Parameters for One-dimensional Reynolds Stress Model
Tao Cai

TL;DR
This study calibrates a one-dimensional Reynolds stress model using 3D simulation data for turbulent compressible convection, successfully reproducing key features like thermal and dissipation layers, and offers practical indicators for stellar modeling.
Contribution
It provides calibrated coefficients for the Reynolds stress model specific to upward overshooting in turbulent convection, validating its application in stellar structure models.
Findings
Calibrated coefficients match pure convection zone values for convection and isotropic terms.
Diffusive coefficients differ significantly, indicating boundary effects.
Reynolds stress model reproduces thermal and dissipation layers seen in 3D simulations.
Abstract
In this paper, we calibrate the coefficients for the one-dimensional Reynolds stress model with the data generated from the three-dimensional numerical simulations of upward overshooting in turbulent compressible convection. It has been found that the calibrated convective and isotropic coefficients are almost the same as those calibrated in the pure convection zone. However, the calibrated diffusive coefficients differ significantly from those calibrated in the pure convection zone. We suspect that the diffusive effect induced by the boundary is stronger than by the adjacent stable zone. We have checked the validity of the downgradient approximation. We find that the prediction of the downgradient approximation on the third-order moments is unsatisfactory. However, the prediction on their derivatives is much better. It explains why the performance of the Reynolds stress model is…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
