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In addition to the bispectral coherence method, phase/time analysis of analytic signals is another promising avenue for the investigation of phase effects in wind waves. Frequency spectra of phase flu...
Asymmetry of wind waves studied in a laboratory tank     Asymmetry of wind waves  laboratory tank       font style='font-size:12px;'> 2009/11/16
Asymmetry of wind waves was studied in laboratory tank tinder varied wind and fetch conditions using both bispectral analysis of wave records and third-order statistics of the surface elevation. It is...
Wind-Generated Current and Phase Speed of Wind Waves     Wind-Generated Current  Phase Speed  Wind Waves       font style='font-size:12px;'> 2009/4/3
Measurements of drift were made in a wind and wave facility at different elevations below the mean water level. The drift profiles were obtained for reference wind speeds, Ur=3.1, 5.7 and 9.6 m sec...
An empirical spectral equation for fetch-limited deep-water wind waves was derived by applying similarity analysis to wind and wave data recorded at the Lake Michigan Research Tower near Muskegon, Mic...
A new method for measuring the directional spectrum, introduced in the preceding paper (Rikiishi, 1978), has been applied to actual wind waves in a large experimental tank 70 m × 8 m with the water 3 ...
It is shown that a simple relation, E* = 5.1 × 10−2 σm*−3 for describing the conditions of growing wind waves, is supported by various available data, where E* = g2E/u*4 is dimensionless e...
Nonlinear Energy Transfer Between Wind Waves     Nonlinear Energy Transfer  Wind Waves       font style='font-size:12px;'> 2009/2/19
A computational scheme for calculating transfer functions is prepared, which gives much improved numerical stability and smoothness compared with previous studies. Besides, a detailed analysis is made...
We analyze in detail the budget of total and fluctuating energy in the surface layer of the ocean. We suggest a rational scheme for separating the budget of turbulence from that of random wind-generat...
It is shown that in order to describe the transfer of gases in the liquid near the air-sea interface, the vertical structure of three-dimensional small-scale turbulence in turbulent patches generated ...
Measurements of the Vertical Acceleration in Wind Waves     Vertical Acceleration  Wind Waves       font style='font-size:12px;'> 2009/1/6
Recent theoretical studies of the accelerations in regular gravity waves of finite steepness have shown striking differences between the Eulerian and the Lagrangian accelerations (those measured by fi...
Equilibrium Spectra of Wind Waves     Wind Waves  Equilibrium Spectra  wind speed       font style='font-size:12px;'> 2008/12/27
Equilibrium spectral behavior for ocean gravity wind waves has been investigated actively over the past three decades, yet fundamental problems remain in reconciling theory with observations. Predicte...
Air Bubbles Produced by Breaking Wind Waves:A Laboratory Study     Air Bubbles  bubble clouds  Wind Waves       font style='font-size:12px;'> 2008/12/27
Air bubbles produced by breaking wind waves are measured in a laboratory tank to study bubble clouds produced in freshwater under various wind and wave conditions. Vertical entrainment of bubbles and ...
A full discrete spectral model for propagation generation and dissipation of wind waves for arbitrary depth, current and wind fields is presented (WAVEWATCH). This model incorporates all relevant wave...
Effects of Tides and Storm Surges on North Sea Wind Waves     Storm Surges  Tides  North Sea Wind Waves       font style='font-size:12px;'> 2008/12/23
Effects of tides and storm surges on wind waves in shelf seas are assessed by hindcasting three North Sea storm cases. It is shown that tides and storm surges in shelf seas should be considered as an ...
Interactions between Rain and Wind Waves     Surface displacement  wind-wave  Rain       font style='font-size:12px;'> 2008/12/22
Effects of rain on surface waves have been investigated in a circulating wind-wave tank. Surface displacement and slope spectra under different wind velocities were measured near the upwind and downwi...

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