Effect of Coriolis force on the linear stability of subaqueous dunes with erodible and non-erodible beds
From MaRDI portal
Publication:2236534
DOI10.1016/j.physleta.2021.127745OpenAlexW3204013289MaRDI QIDQ2236534
Publication date: 25 October 2021
Published in: Physics Letters. A (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.physleta.2021.127745
Cites Work
- Unnamed Item
- Unnamed Item
- Complete group classification of the two-dimensional shallow water equations with constant Coriolis parameter in Lagrangian coordinates
- Symmetric and asymmetric inertial instability of zonal jets on the -plane with complete Coriolis force
- Multilayer shallow water equations with complete Coriolis force. Part 2. Linear plane waves
- Hydrodynamic Instabilities
- The phase lead of shear stress in shallow-water flow over a perturbed bottom
- Shallow water equations with a complete Coriolis force and topography
- Multilayer shallow water equations with complete Coriolis force. Part 1. Derivation on a non-traditional beta-plane
- General stability conditions for zonal flows in a one-layer model on the β-plane or the sphere
- The formation of ripples and dunes on an erodible bed
- Revisiting the linear theory of sand dune formation
- Wave propagation and boundary instability in erodible-bed channels
- The mechanics of dunes and antidunes in erodible-bed channels
This page was built for publication: Effect of Coriolis force on the linear stability of subaqueous dunes with erodible and non-erodible beds