An Experimental Investigation of Wind-generated Waves PDF Download
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Author: Joe William Johnson
Publisher:
ISBN:
Category : Wind waves
Languages : en
Pages : 44
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Book Description
Author: Joe William Johnson
Publisher:
ISBN:
Category : Wind waves
Languages : en
Pages : 44
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Book Description
Author: Harold von Neufville Flinsch
Publisher:
ISBN:
Category : Waves
Languages : en
Pages : 166
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Book Description
Author: Carsten Hansen
Publisher:
ISBN:
Category :
Languages : en
Pages : 147
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Book Description
Author: Hui Chuan Liang
Publisher:
ISBN:
Category : Wind waves
Languages : en
Pages : 238
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Book Description
Author: Susumu Karaki
Publisher:
ISBN:
Category : Ocean waves
Languages : en
Pages : 126
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Book Description
This investigation presents experimental results from a study of the structure of a turbulent boundary layer developed by air flow over water waves in a lab wind-wave channel. It was demonstrated that the sheared flow region is two-layered, similar to rough wall boundary layers. The inner layer, adjacent to the wall, is describable by the 'law of the wall' and the outer flow by the 'defect law.' The data were taken in two-dimensional flow with small favorable pressure gradients. The first part of the two-part investigation involved air flow over an initially still water surface on which waves developed in response to wind excitation. In the second part, air was passed over water waves of a single frequency and varied amplitude. The results indicated that within the range of this study the water surface can be classed as aerodynamically rough at wind speeds greater than 12 fps and the flow structure of the boundary layer corresponds to that over a rough wall. The velocity decrement due to surface roughness is shown to be a function of the local root-mean-square wave height. The effect of wave-induced fluctuations in the air is limited to a very close neighborhood of the wavy surface. For the specific combination of wind and wave speeds of this study it was found that while the amplitudes of the horizontal components of the fluctuation decreased with increasing elevation, the vertical component increased. (Author).
Author: Richard Ives Hires
Publisher:
ISBN:
Category : Ocean-atmosphere interaction
Languages : en
Pages : 192
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Book Description
An experimental investigation was made to determine the ratio of the wave-supported shear stress, phi sub w; to the total shear stress on the water surface, phi sub o. The experimental conditions were designed to correspond to those required for the application of the viscous shear flow theory of wave generation proposed by Brooke Benjamin (1959) and Miles (1962b). The experiments were performed in a wind-wave tunnel, 48 x 3-1/2 x 2 feet, with a mean water depth of 1-1/2 feet. The wind in the 6 in. air space above the water was fully-developed turbulent channel flow. The mean center-line wind speed, U sub xi, was kept constant at 1.20 m/s during all measurements made with the wind blowing over the water. An artificially generated, single-component, wave train of small amplitude provided a known, initial perturbation of the water surface with which the wind could interact. The range of wave frequencies investigated was from 4.0 to 5.2 cps. Wave measurements were made with capacitance wave probes, wind measurements with hot-wire anemometers. (Author).
Author: W. Stanley Wilson
Publisher:
ISBN:
Category : Ocean waves
Languages : en
Pages : 110
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Book Description
An experimental study was conducted to measure the growth rates of mechanically generated surface water waves when subjected to fully developed turbulent channel airflow. The study was designed to test the accuracy of the growth rates predicted by the Miles; 1962 Theory. (Author).
Author: Andrey Zavadsky
Publisher:
ISBN:
Category :
Languages : en
Pages : 117
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Book Description
Author: Charles L. Bretschneider
Publisher:
ISBN:
Category : Wind waves
Languages : en
Pages : 44
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Book Description
Author: Timothy P. Barnett
Publisher:
ISBN:
Category :
Languages : en
Pages : 30
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Book Description
A 2-year field study of the mechanisms of wind wave generation and dissipation has been conducted in the North Sea. The study is a multi-nation effort. The experimental techniques and layout are described. The quality and quantity of data collected were good in 1968 and excellent in 1969. The results derived from these data are not discussed. (Author).
