On the instability of some upward propagating, exact, nonlinear mountain waves
Fuente:
arXiv
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| Formato: | Preprint |
| Publicado: |
2026
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| _version_ | 1866911567645245440 |
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| author | Puntini, Christian |
| author_facet | Puntini, Christian |
| contents | Using the short-wavelength instability method, we investigate the linear instability of an exact solution describing upward-propagating mountain waves, derived in A. Constantin, \emph{J. Phys. A: Math. Theor.} (2023), under the assumption of a dry adiabatic flow. Within this approach, the stability problem reduces to analysing a system of ordinary differential equations along fluid trajectories. Our results show that the flow becomes unstable when the wave steepness exceeds the critical threshold of $\frac{1}{3}$. Given the representation of the solution in Lagrangian coordinates, the instability analysis will show the existence of an unstable layer of few hundred meters beneath the tropopause where instability may occur, finally leading to a chaotic 3-dimensional fluid motion. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2604_03620 |
| institution | arXiv |
| publishDate | 2026 |
| record_format | arxiv |
| spellingShingle | On the instability of some upward propagating, exact, nonlinear mountain waves Puntini, Christian Atmospheric and Oceanic Physics Mathematical Physics Analysis of PDEs Dynamical Systems Fluid Dynamics 76N30, 76E20, 86A10 Using the short-wavelength instability method, we investigate the linear instability of an exact solution describing upward-propagating mountain waves, derived in A. Constantin, \emph{J. Phys. A: Math. Theor.} (2023), under the assumption of a dry adiabatic flow. Within this approach, the stability problem reduces to analysing a system of ordinary differential equations along fluid trajectories. Our results show that the flow becomes unstable when the wave steepness exceeds the critical threshold of $\frac{1}{3}$. Given the representation of the solution in Lagrangian coordinates, the instability analysis will show the existence of an unstable layer of few hundred meters beneath the tropopause where instability may occur, finally leading to a chaotic 3-dimensional fluid motion. |
| title | On the instability of some upward propagating, exact, nonlinear mountain waves |
| topic | Atmospheric and Oceanic Physics Mathematical Physics Analysis of PDEs Dynamical Systems Fluid Dynamics 76N30, 76E20, 86A10 |
| url | https://arxiv.org/abs/2604.03620 |