arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2008.08467physics.flu-dynnlin.CDphysics.class-ph
收藏

Saturation of the inverse cascade in surface gravity wave turbulence

Eric Falcon, Guillaume Michel, Gaurav Prabhudesai, Annette Cazaubiel, Michaël Berhanu, Nicolas Mordant, Sébastien Aumaitre, F. Bonnefoy

英文摘要:

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.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑