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dc.contributor.authorAndrassy, R
dc.contributor.authorHigl, J
dc.contributor.authorMao, H
dc.contributor.authorMocák, M
dc.contributor.authorVlaykov, DG
dc.contributor.authorArnett, WD
dc.contributor.authorBaraffe, I
dc.contributor.authorCampbell, SW
dc.contributor.authorConstantino, T
dc.contributor.authorEdelmann, PVF
dc.contributor.authorGoffrey, T
dc.contributor.authorGuillet, T
dc.contributor.authorHerwig, F
dc.contributor.authorHirschi, R
dc.contributor.authorHorst, L
dc.contributor.authorLeidi, G
dc.contributor.authorMeakin, C
dc.contributor.authorPratt, J
dc.contributor.authorRizzuti, F
dc.contributor.authorRöpke, FK
dc.contributor.authorWoodward, P
dc.date.accessioned2022-04-12T14:29:40Z
dc.date.issued2022-03-28
dc.date.updated2022-04-12T14:00:43Z
dc.description.abstractOur ability to predict the structure and evolution of stars is in part limited by complex, 3D hydrodynamic processes such as convective boundary mixing. Hydrodynamic simulations help us understand the dynamics of stellar convection and convective boundaries. However, the codes used to compute such simulations are usually tested on extremely simple problems and the reliability and reproducibility of their predictions for turbulent flows is unclear. We define a test problem involving turbulent convection in a plane-parallel box, which leads to mass entrainment from, and internal-wave generation in, a stably stratified layer. We compare the outputs from the codes FLASH, MUSIC, PPMSTAR, PROMPI, and SLH, which have been widely employed to study hydrodynamic problems in stellar interiors. The convection is dominated by the largest scales that fit into the simulation box. All time-averaged profiles of velocity components, fluctuation amplitudes, and fluxes of enthalpy and kinetic energy are within ≲3σ of the mean of all simulations on a given grid (1283 and 2563 grid cells), where σ describes the statistical variation due to the flow’s time dependence. They also agree well with a 5123 reference run. The 1283 and 2563 simulations agree within 9% and 4%, respectively, on the total mass entrained into the convective layer. The entrainment rate appears to be set by the amount of energy that can be converted to work in our setup and details of the small-scale flows in the boundary layer seem to be largely irrelevant. Our results lend credence to hydrodynamic simulations of flows in stellar interiors. We provide in electronic form all outputs of our simulations as well as all information needed to reproduce or extend our study.en_GB
dc.description.sponsorshipScience and Technology Facilities Council (STFC)en_GB
dc.description.sponsorshipEuropean Research Council (ERC)en_GB
dc.format.extenta193-
dc.identifier.citationVol. 659, article a193en_GB
dc.identifier.doihttps://doi.org/10.1051/0004-6361/202142557
dc.identifier.grantnumberST/R000395/1en_GB
dc.identifier.grantnumber787361en_GB
dc.identifier.urihttp://hdl.handle.net/10871/129367
dc.identifierORCID: 0000-0001-8365-5982 (Baraffe, I)
dc.identifierORCID: 0000-0002-0271-5953 (Guillet, T)
dc.language.isoenen_GB
dc.publisherEuropean Southern Observatory (ESO) / EDP Sciencesen_GB
dc.rights© ESO 2022en_GB
dc.subjecthydrodynamicsen_GB
dc.subjectconvectionen_GB
dc.subjectturbulenceen_GB
dc.subjectstars: interiorsen_GB
dc.subjectmethods: numericalen_GB
dc.titleDynamics in a stellar convective layer and at its boundary: Comparison of five 3D hydrodynamics codesen_GB
dc.typeArticleen_GB
dc.date.available2022-04-12T14:29:40Z
dc.identifier.issn0004-6361
dc.descriptionThis is the final version. Available from EDP Sciences via the DOI in this recorden_GB
dc.identifier.eissn1432-0746
dc.identifier.journalAstronomy & Astrophysicsen_GB
dc.relation.ispartofAstronomy & Astrophysics, 659
dc.rights.urihttp://www.rioxx.net/licenses/all-rights-reserveden_GB
dcterms.dateAccepted2021-12-29
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2022-03-28
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2022-04-12T14:26:11Z
refterms.versionFCDVoR
refterms.dateFOA2022-04-12T14:29:52Z
refterms.panelBen_GB
refterms.dateFirstOnline2022-03-28


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