G714 Estimate of wave length at extremely high wind speeds
Naohisa Takagaki, Takenori Kuramoto, Hiroyuki KAMIUCHI, Koji Iwano, Ryoichi Kurose, Satoru Komori
Abstract
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Naohisa Takagaki, Takenori Kuramoto, Hiroyuki KAMIUCHI, Koji Iwano, Ryoichi Kurose, Satoru Komori
Abstract
Open-access reader
Wave slope was evaluated by measuring both significant wave height and length in a broad wind speed range. Experiments were conducted in a high-speed wind wave tank. The results show that the significant wave length increases steeply with free-stream wind-speed at low wind speeds ( U_∞ <15 m/s), increases gradually at middle wind speeds (15 ≦ U_∞ < 27 m/s), and increases steeply again at extremely high wind speeds (U_∞>= 27 m/s). The wave slope increases with the free-stream wind-speed in the low wind speed region ( U_∞ <15 m/s), but it reaches a constant value in the high wind speed region (U_∞ ≧ 15 m/s). These results suggest that the trend of wave development in the high wind speed region is different from that in the low wind speed region owing to wave breaking.
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Wave slope was evaluated by measuring both significant wave height and length in a broad wind speed range. Experiments were conducted in a high-speed wind wave tank. The results show that the significant wave length increases steeply with free-stream wind-speed at low wind speeds ( U_∞ <15 m/s), increases gradually at middle wind speeds (15 ≦ U_∞ < 27 m/s), and increases steeply again at extremely high wind speeds (U_∞>= 27 m/s). The wave slope increases with the free-stream wind-speed in the low wind speed region ( U_∞ <15 m/s), but it reaches a constant value in the high wind speed region (U_∞ ≧ 15 m/s). These results suggest that the trend of wave development in the high wind speed region is different from that in the low wind speed region owing to wave breaking.
Key concepts: Wind speed, Wind gradient, Wind profile power law, Wave speed, Meteorology, Maximum sustained wind, Wave height, Range (aeronautics)