Inhomogeneity-induced wavenumber diffusion
Year: 2025
Type: article
Abstract: Inertia–gravity waves are scattered by background flows as a result of Doppler shift by a non-uniform velocity. In the Wentzel–Kramers–Brillouin regime, the scattering process reduces to a diffusion in spectral space. Other inhomogeneities that the waves encounter, such as density variations, also cause scattering and spectral diffusion. We generalise the spectral diffusion equation to account for these inhomogeneities. We apply the result to a rotating shallow-water system, for which height inhomogeneities arise from velocity inhomogeneities through geostrophy, and to the Boussinesq system for which buoyancy inhomogeneities arise similarly. We compare the contributions that height and buoyancy variations make to the spectral diffusion with the contribution of the Doppler shift. In both systems, we find regimes where all contributions are significant. We support our findings with exact solutions of the diffusion equation and with ray tracing simulations in the shallow-water case.
Source: Journal of Fluid Mechanics
DOI: 10.1017/jfm.2025.23
Language: English
Subfield: Oceanography
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: hybrid
Estimated APC paid: $3,550
Awards: Phase Averaged Deferred Correction for Multi-Timescale Systems, G2841395204, G5873782705, Computing Lagrangian means in multi-timescale fluid flows, NSFGEO-NERC Scattering of ocean surface gravity waves by submesoscale turbulence, EPSRC Centre for Doctoral Training in Mathematical Modelling, Analysis and Computation (MAC-MIGS)
OpenAlex ID: W4408462257
