2019
DOI: 10.1142/s0218202520500037
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On the wave turbulence theory for stratified flows in the ocean

Abstract: After the pioneering work of Garrett and Munk, the statistics of oceanic internal gravity waves has become a central subject of research in oceanography. The time evolution of the spectral energy of internal waves in the ocean can be described by a near-resonance wave turbulence equation, of quantum Boltzmann type. In this work, we provide the first rigorous mathematical study for the equation by showing the global existence and uniqueness of strong solutions.

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Cited by 24 publications
(21 citation statements)
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References 70 publications
(82 reference statements)
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“…In addition, our local approach provides an efficient way to numerically investigate the detailed and possibly universal properties of weakly forced internal wave turbulence in low dissipation regimes. Despite recent experimental ) and theoretical ([Gamba et al, 2017]) advances, this particular state of stratified turbulence remains challenging and difficult to be compared to the classical theory of wave turbulence ( [Zakharov et al, 1992, Nazarenko, 2011). As in rotating turbulence, this is essentially due to the anisotropy of the dispersion relation (see for instance the discussion in ), the role played by nearresonant interactions and the non-linear interaction with non-propagative modes ( [Cambon, 2001, Galtier, 2003, Smith and Lee, 2005, Bellet et al, 2006, Scott, 2014, Gelash et al, 2017, Gamba et al, 2017).…”
Section: Resultsmentioning
confidence: 99%
“…In addition, our local approach provides an efficient way to numerically investigate the detailed and possibly universal properties of weakly forced internal wave turbulence in low dissipation regimes. Despite recent experimental ) and theoretical ([Gamba et al, 2017]) advances, this particular state of stratified turbulence remains challenging and difficult to be compared to the classical theory of wave turbulence ( [Zakharov et al, 1992, Nazarenko, 2011). As in rotating turbulence, this is essentially due to the anisotropy of the dispersion relation (see for instance the discussion in ), the role played by nearresonant interactions and the non-linear interaction with non-propagative modes ( [Cambon, 2001, Galtier, 2003, Smith and Lee, 2005, Bellet et al, 2006, Scott, 2014, Gelash et al, 2017, Gamba et al, 2017).…”
Section: Resultsmentioning
confidence: 99%
“…where the integral is defined in the sense of (33). Observe that ξ in the integral is taken within the interval [p 1 , p 1 + p 2 ], then 1…”
Section: Let Us Now Estimatementioning
confidence: 99%
“…Besides the 4-wave kinetic equation, the 3-wave kinetic equation also plays an important role in the theory of weak turbulence, and has been studied in [16,2,23,11,15] for the phonon interactions in anharmonic crystal lattices, in [23] for stratified flows in the ocean, and in [48] for capillary waves.…”
Section: Rigorous Results On the Isotropic 4-wave Kinetic Equation Anmentioning
confidence: 99%