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IMPROVED ESTIMATES OF SWELL FROM MOORED BUOYS

机译:改进了停泊浮标的膨胀估计

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摘要

The National Data Buoy Center (NDBC) began posting buoy estimates of swell height and period in 1997 because of numerous requests from mariners. Until then, only significant wave height, dominant period, and spectral wave data were posted on its Web site. Though swell information can be gleaned from the wave energy spectral, many mariners do not have the time or experience to do so. NDBC developed a method based on wave steepness that requires only nondirectional wave data. This method determines a period to separate the wind seas from the swell based on the knowledge that seas are steeper than swell and that maximum steepness occurs near the peak period of the wind waves. However, the method underestimates the swell when winds are light or abating, as compared to the Navy's operational wave model (WAM). To improve performance, the steepness method was modified to limit the maximum allowable separation period based on the observed wind speed. Since peak frequencies of fully developed seas generated by a given wind speed are well known, this relationship can be used to set an upper limit on the separation period. Positive results were obtained in tests of the modified method using measurements from directional buoys where swell and wind seas can be easily identified by differences in propagation direction. The modified method also compared much more favorably with wind sea and swell estimates from the WAM.
机译:国家数据浮标中心(NDBC)开始发布1997年膨胀高度和期间的浮标估计,因为来自水手的许多要求。在此之前,仅在其网站上发布了显着的波形高度,主导时段和光谱波数据。虽然可以从波能量谱中收集膨胀信息,但是许多水手没有时间或经验。 NDBC开发了一种基于波陡度的方法,该方法仅需要非向波浪数据。该方法基于海洋陡峭的知识,确定了将风海与膨胀相比分开的时期,并且在风波的峰值周期附近发生最大陡峭。然而,与海军的操作波模型(WAM)相比,该方法低估了风光或减弱时膨胀。为了提高性能,修改陡峭方法以限制基于观察到的风速的最大允许分离时段。由于通过给定风速产生的完全发育海的峰值频率是众所周知的,因此这种关系可用于在分离时段的上限设置上限。在使用从方向浮标的定向浮标的测量的测试方法中获得了阳性结果,其中可以通过传播方向的差异容易地识别出膨胀和风海。改性方法也与风海相比更有利,从旺旺威胁蔓延。

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