Saturation of the Inverse Cascade in Surface Gravity-Wave Turbulence

E. Falcon, G. Michel, G. Prabhudesai, A. Cazaubiel, M. Berhanu, N. Mordant, S. Aumaître, and F. Bonnefoy
Phys. Rev. Lett. 125, 134501 – Published 21 September 2020
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Abstract

We report on the observation of surface gravity-wave turbulence at scales larger than the forcing ones in a large basin. In addition to the downscale transfer usually reported in gravity-wave turbulence, an upscale transfer is observed, interpreted as the inverse cascade of weak turbulence theory. A steady state is achieved when the inverse cascade reaches a scale in between the forcing wavelength and the basin size, but far from the latter. This inverse cascade saturation, which depends on the wave steepness, is probably due to the emergence of nonlinear dissipative structures such as sharp-crested waves.

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  • Received 4 May 2020
  • Accepted 14 August 2020

DOI:https://doi.org/10.1103/PhysRevLett.125.134501

© 2020 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

E. Falcon1,*, G. Michel2, G. Prabhudesai3, A. Cazaubiel1, M. Berhanu1, N. Mordant4, S. Aumaître5, and F. Bonnefoy6

  • 1Université de Paris, Univ Paris Diderot, MSC, UMR 7057 CNRS, F-75 013 Paris, France
  • 2Sorbonne Université, IJLRA, UMR 7190 CNRS, F-75 005 Paris, France
  • 3Ecole Normale Supérieure, LPS, UMR 8550 CNRS, F-75 205 Paris, France
  • 4Université Grenoble Alpes, LEGI, UMR 5519 CNRS, F-38 000 Grenoble, France
  • 5CEA-Saclay, Sphynx, DSM, URA 2464 CNRS, F-91 191 Gif-sur-Yvette, France
  • 6Ecole Centrale de Nantes, LHEEA, UMR 6598 CNRS, F-44 321 Nantes, France

  • *eric.falcon@univ-paris-diderot.fr

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Issue

Vol. 125, Iss. 13 — 25 September 2020

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