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Buoy Measurements of Wind-Wave Relations during Hurricane Matthew in 2016

机译:2016年马修飓风期间风波关系的浮标测量

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Studies suggested that neutral-stability wind speed at 10 m U-10 >= 9 m s(-1) and wave steepness H-s/L-p >= 0.020 can be taken as criteria for aerodynamically rough ocean surface and the onset of a wind sea, respectively; here, H-s is the significant wave height, and L-p is the peak wavelength. Based on these criteria, it is found that, for the growing wind seas when the wave steepness increases with time during Hurricane Matthew in 2016 before the arrival of its center, the dimensionless significant wave height and peak period is approximately linearly related, resulting in U-10 = 35H(s)/T-p; here, T-p is the dominant or peak wave period. This proposed wind-wave relation for aerodynamically rough flow over the wind seas is further verified under Hurricane Ivan and North Sea storm conditions. However, after the passage of Matthew's center, when the wave steepness was nearly steady, a power-law relation between the dimensionless wave height and its period prevailed with its exponent equal to 1.86 and a very high correlation coefficient of 0.97.
机译:研究表明,在10 m U-10> = 9 ms(-1)下的中性稳定风速和波速Hs / Lp> = 0.020可以分别作为空气动力学粗糙海洋表面和风海开始的标准;在这里,H-s是有效波高,L-p是峰值波长。根据这些标准,发现对于风速不断增长的风海,当马修飓风在其中心到达之前的2016年期间,波的陡度随时间增加时,无量纲的有效波高和峰值周期近似线性相关,从而导致U -10 = 35H(s)/ Tp;在这里,T-p是主导或峰值波周期。在飓风“伊万”和北海风暴条件下,对风浪在空气动力学上粗糙流动的拟议风波关系得到了进一步验证。然而,在马修中心通过之后,当波陡度几乎稳定时,无量纲波高与其周期之间的幂律关系占主导地位,其指数等于1.86,相关系数非常高,为0.97。

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  • 来源
    《Journal of Physical Oceanography》 |2017年第10期|2603-2609|共7页
  • 作者

    Hsu S. A.; He Yijun; Shen Hui;

  • 作者单位

    Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing, Jiangsu, Peoples R China|Louisiana State Univ, Coastal Studies Inst, Baton Rouge, LA 70803 USA|Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA;

    Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing, Jiangsu, Peoples R China|Bedford Inst Oceanog, Dartmouth, NS, Canada;

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