Loop-Type Wave-Generation Method for Generating Wind Waves under Long-Fetch Conditions

AbstractIt is important to develop a wave-generation method for extending the fetch in laboratory experiments, because previous laboratory studies were limited to the fetch shorter than several dozen meters. A new wave-generation method is proposed for generating wind waves under long-fetch conditions in a wind-wave tank, using a programmable irregular-wave generator. This new method is named a loop-type wave-generation method (LTWGM), because the waves with wave characteristics close to the wind waves measured at the end of the tank are reproduced at the entrance of the tank by the programmable irregular-wave generator and the mechanical wave generation is repeated at the entrance in order to increase the fetch. Water-level fluctuation is measured at both normal and extremely high wind speeds using resistance-type wave gauges. The results show that, at both wind speeds, LTWGM can produce wind waves with long fetches exceeding the length of the wind-wave tank. It is observed that the spectrum of wind wave...

[1]  R. Kurose,et al.  Mechanism of drag coefficient saturation at strong wind speeds , 2016 .

[2]  R. Kurose,et al.  Direct numerical simulation of turbulent heat transfer across a sheared wind-driven gas–liquid interface , 2016, Journal of Fluid Mechanics.

[3]  S. Komori,et al.  Estimation of friction velocity from the wind-wave spectrum at extremely high wind speeds , 2016 .

[4]  R. Kurose,et al.  Effects of turbulent eddies and Langmuir circulations on scalar transfer in a sheared wind-driven liquid flow , 2015 .

[5]  B. Jähne,et al.  First laboratory study of air–sea gas exchange at hurricane wind speeds , 2014 .

[6]  R. Kurose,et al.  Mass transfer velocity across the breaking air–water interface at extremely high wind speeds , 2013 .

[7]  R. Kurose,et al.  Strong correlation between the drag coefficient and the shape of the wind sea spectrum over a broad range of wind speeds , 2012 .

[8]  Y. Troitskaya,et al.  Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions , 2012 .

[9]  R. Burling SURFACE WAVES ON ENCLOSED BODIES OF WATER , 2011 .

[10]  W. Melville,et al.  Airborne Observations of Fetch-Limited Waves in the Gulf of Tehuantepec , 2010 .

[11]  S. Komori,et al.  Effects of rainfall on mass transfer across the air‐water interface , 2007 .

[12]  Nicolas Reul,et al.  On the limiting aerodynamic roughness of the ocean in very strong winds , 2004 .

[13]  M. Powell,et al.  Reduced drag coefficient for high wind speeds in tropical cyclones , 2003, Nature.

[14]  Anatol D. Rozenberg,et al.  Free and bound capillary waves as microwave scatterers: laboratory studies , 1999, IEEE Trans. Geosci. Remote. Sens..

[15]  S. Larsen,et al.  On the Dependence of Sea Surface Roughness on Wind Waves , 1998 .

[16]  Yasuhiro Murakami,et al.  Turbulence structure and mass transfer across a sheared air–water interface in wind-driven turbulence , 1993, Journal of Fluid Mechanics.

[17]  H. Mitsuyasu,et al.  On the dispersion relation of random gravity waves. Part 2. An experiment , 1979, Journal of Fluid Mechanics.

[18]  Yoshiaki Toba,et al.  Local balance in the air-sea boundary processes , 1973 .

[19]  Yoshiaki Toba,et al.  Local balance in the air-sea boundary processes , 1972 .

[20]  H. Hawkins,et al.  HURRICANE HILDA, 1964 , 1968 .

[21]  F. H. Hawkins,et al.  Hurricane Hilda, 1964 II. Structure and Budgets of the Hurricane on October 1, 1964 , 1968 .

[22]  B. W. Wilson,et al.  Numerical prediction of ocean waves in the North Atlantic for December, 1959 , 1965 .

[23]  W. Pierson,et al.  A proposed spectral form for fully developed wind seas based on the similarity theory of S , 1964 .

[24]  O. Phillips The equilibrium range in the spectrum of wind-generated waves , 1958, Journal of Fluid Mechanics.

[25]  Donald T. Resio,et al.  Equilibrium‐range constant in wind‐generated wave spectra , 2004 .