2D Internal Gravity Wave Turbulence
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arXiv
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| Auteurs principaux: | , |
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| Format: | Preprint |
| Publié: |
2024
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| _version_ | 1866912984493719552 |
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| author | Labarre, Vincent Shavit, Michal |
| author_facet | Labarre, Vincent Shavit, Michal |
| contents | Using weak wave turbulence theory analysis, we distinguish three main regimes for 2D stratified fluids in the dimensionless parameter space defined by the Froude number and the Reynolds number: discrete wave turbulence, weak wave turbulence, and strong nonlinear interaction. These regimes are investigated using direct numerical simulations (DNS) of the 2D Boussinesq equations with shear modes removed. In the weak wave turbulence regime, excluding slow frequencies, we observe a spectrum that aligns with recent predictions from kinetic theory. This finding represents the first DNS-based confirmation of wave turbulence theory for internal gravity waves. At strong stratification, in both the weak and strong interaction regimes, we observe the formation of layers accompanied by spectral peaks at low discrete frequencies. We explain this layering through an inverse kinetic energy cascade and the discreteness of wave-wave interactions at large scales. This analysis allows us to predict the layer thickness and typical flow velocity in terms of the control parameters. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2412_20534 |
| institution | arXiv |
| publishDate | 2024 |
| record_format | arxiv |
| spellingShingle | 2D Internal Gravity Wave Turbulence Labarre, Vincent Shavit, Michal Fluid Dynamics Using weak wave turbulence theory analysis, we distinguish three main regimes for 2D stratified fluids in the dimensionless parameter space defined by the Froude number and the Reynolds number: discrete wave turbulence, weak wave turbulence, and strong nonlinear interaction. These regimes are investigated using direct numerical simulations (DNS) of the 2D Boussinesq equations with shear modes removed. In the weak wave turbulence regime, excluding slow frequencies, we observe a spectrum that aligns with recent predictions from kinetic theory. This finding represents the first DNS-based confirmation of wave turbulence theory for internal gravity waves. At strong stratification, in both the weak and strong interaction regimes, we observe the formation of layers accompanied by spectral peaks at low discrete frequencies. We explain this layering through an inverse kinetic energy cascade and the discreteness of wave-wave interactions at large scales. This analysis allows us to predict the layer thickness and typical flow velocity in terms of the control parameters. |
| title | 2D Internal Gravity Wave Turbulence |
| topic | Fluid Dynamics |
| url | https://arxiv.org/abs/2412.20534 |