Transition to turbulence at the bottom of a solitary wave

被引:15
|
作者
Blondeaux, Paolo [1 ]
Pralits, Jan [1 ]
Vittori, Giovanna [1 ]
机构
[1] Univ Genoa, Dept Civil Environm & Architectural Engn, I-16145 Genoa, Italy
关键词
boundary layer stability; coastal engineering; solitary waves; OSCILLATORY BOUNDARY-LAYERS; COHERENT STRUCTURES; DIRECT SIMULATION; FLOWS; STABILITY; MECHANISM;
D O I
10.1017/jfm.2012.341
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A linear stability analysis of the laminar flow in the boundary layer at the bottom of a solitary wave is made to determine the conditions leading to transition and the appearance of turbulence. The Reynolds number of the phenomenon is assumed to be large and a 'momentary' criterion of instability is used. The results show that the laminar regime becomes unstable during the decelerating phase, when the height of the solitary wave exceeds a threshold value which depends on the ratio between the boundary layer thickness and the local water depth. A comparison of the theoretical results with the experimental measurements of Sumer et al. (J. Fluid Mech., vol. 646, 2010, pp. 207-231) supports the analysis.
引用
收藏
页码:396 / 407
页数:12
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