Abstract
In the present work the possibility of turbulence closure applying to improve barotropic jet instability simulation at coarse grid resolutions is considered. This problem is analogous to situations occurring in eddy-permitting ocean models when Rossby radius of deformation is partly resolved on a computational grid. We show that the instability is slowed down at coarse resolutions. As follows from the spectral analysis of linearized equations, the slowdown is caused by the small-scale normal modes damping arising due to numerical approximation errors and nonzero eddy viscosity. In order to accelerate instability growth, stochastic and deterministic kinetic energy backscatter (KEBs) parameterizations and scale-similarity model were applied. Their utilization led to increase of the growth rates of normal modes and thus improve characteristic time and spatial structure of the instability.
Acknowledgment
Author would like to thank A. V. Glazunov, V. P. Dymnikov, and Yu. M. Nechepurenko for helpful comments and discussion.
Funding: This work was supported by the Russian Foundation for Basic Research (projects {19-35-90023, break 18-05-60184).
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© 2020 Walter de Gruyter GmbH, Berlin/Boston
Articles in the same Issue
- Frontmatter
- Modelling of equatorial ionospheric anomaly in the INM RAS coupled thermosphere-ionosphere model
- The study of time dependence of particle flux with multiplication in a random medium
- 2D turbulence closures for the barotropic jet instability simulation
- Large-scale structures in stratified turbulent Couette flow and optimal disturbances
Articles in the same Issue
- Frontmatter
- Modelling of equatorial ionospheric anomaly in the INM RAS coupled thermosphere-ionosphere model
- The study of time dependence of particle flux with multiplication in a random medium
- 2D turbulence closures for the barotropic jet instability simulation
- Large-scale structures in stratified turbulent Couette flow and optimal disturbances