Effective drift velocity from turbulent transport by vorticity
Abstract
We highlight the differing roles of vorticity and strain in the transport of coarse-grained scalars at length-scales larger than l by smaller scale (subscale) turbulence. We use the first term in a multiscale gradient expansion due to Eyink [1], which exhibits excellent correlation with the exact subscale physics when the partitioning length l is any scale smaller than that of the spectral peak. We show that unlike subscale strain, which acts as an anisotropic diffusion/anti-diffusion tensor, subscale vorticity’s contribution is solely a conservative advection of coarse-grained quantities by an eddy-induced non-divergent velocity, v*, that is proportional to the curl of vorticity. Therefore, material (Lagrangian) advection of coarse-grained quantities is accomplished not by the coarse grained flow velocity, u , but by the effective velocity, u + v*, the physics of which may improve commonly used LES models.
- Authors:
-
- Univ. of Rochester, NY (United States)
- NOAA/Geophysical Fluid Dynamics Lab., Princeton, NJ (United States); Princeton Univ. Program in Atmospheric and Oceanic Sciences, NJ (United States)
- Publication Date:
- Research Org.:
- Univ. of Rochester, NY (United States). Lab. for Laser Energetics
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA); National Science Foundation (NSF); National Aeronautics and Space Administration (NASA)
- OSTI Identifier:
- 1890485
- Alternate Identifier(s):
- OSTI ID: 1903295; OSTI ID: 1957732
- Grant/Contract Number:
- SC0020229; SC0019329; CBET-2143702; PHY-2020249; PHY-2206380; OCE-2123496; 80NSSC18K0772; NA0003856; SC0014318; NA0003914; AC02-05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Physical Review Fluids (Online)
- Additional Journal Information:
- Journal Name: Physical Review Fluids (Online); Journal Volume: 7; Journal Issue: 10; Journal ID: ISSN 2469-990X
- Publisher:
- American Physical Society (APS)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 42 ENGINEERING; Astrophysical fluid dynamics; Geophysical fluid dynamics; Turbulence; Chaos & nonlinear dynamics; Navier-Stokes equation
Citation Formats
Aluie, Hussein, Rai, Shikhar, Yin, Hao, Lees, Aarne, Zhao, Dongxiao, Griffies, Stephen M., Adcroft, Alistair, and Shang, Jessica K. Effective drift velocity from turbulent transport by vorticity. United States: N. p., 2022.
Web. doi:10.1103/physrevfluids.7.104601.
Aluie, Hussein, Rai, Shikhar, Yin, Hao, Lees, Aarne, Zhao, Dongxiao, Griffies, Stephen M., Adcroft, Alistair, & Shang, Jessica K. Effective drift velocity from turbulent transport by vorticity. United States. https://doi.org/10.1103/physrevfluids.7.104601
Aluie, Hussein, Rai, Shikhar, Yin, Hao, Lees, Aarne, Zhao, Dongxiao, Griffies, Stephen M., Adcroft, Alistair, and Shang, Jessica K. Mon .
"Effective drift velocity from turbulent transport by vorticity". United States. https://doi.org/10.1103/physrevfluids.7.104601. https://www.osti.gov/servlets/purl/1890485.
@article{osti_1890485,
title = {Effective drift velocity from turbulent transport by vorticity},
author = {Aluie, Hussein and Rai, Shikhar and Yin, Hao and Lees, Aarne and Zhao, Dongxiao and Griffies, Stephen M. and Adcroft, Alistair and Shang, Jessica K.},
abstractNote = {We highlight the differing roles of vorticity and strain in the transport of coarse-grained scalars at length-scales larger than l by smaller scale (subscale) turbulence. We use the first term in a multiscale gradient expansion due to Eyink [1], which exhibits excellent correlation with the exact subscale physics when the partitioning length l is any scale smaller than that of the spectral peak. We show that unlike subscale strain, which acts as an anisotropic diffusion/anti-diffusion tensor, subscale vorticity’s contribution is solely a conservative advection of coarse-grained quantities by an eddy-induced non-divergent velocity, v*, that is proportional to the curl of vorticity. Therefore, material (Lagrangian) advection of coarse-grained quantities is accomplished not by the coarse grained flow velocity, u , but by the effective velocity, u + v*, the physics of which may improve commonly used LES models.},
doi = {10.1103/physrevfluids.7.104601},
journal = {Physical Review Fluids (Online)},
number = 10,
volume = 7,
place = {United States},
year = {Mon Oct 03 00:00:00 EDT 2022},
month = {Mon Oct 03 00:00:00 EDT 2022}
}
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