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Validation of operational global wave prediction models with spectral buoy data

机译:用频谱浮标数据验证运行中的全球波浪预测模型

摘要

Global wave predictions produced at two U. S. forecasting centers, Fleet Numerical Meteorology and Oceanography Center and the National Centers for Environmental Prediction are evaluated with spectral buoy measurements. In this study, the fidelity of frequency-directional spectra predicted by WAM and WAVEWATCH III at the operational centers is examined with data from 3-meter discus and 6-meter nomad buoys operated by the National Data Buoy Center in the Atlantic and Pacific Oceans and Datawell Directional Waverider buoys deployed along the California coast by the Scripps Institution of Oceanography Coastal Data Information Program. Only buoys located in deep water are used in the comparisons. Model nowcasts of frequency spectra and mean wave directions are compared to buoy measurements over a six-month period from 1 October 2000 to 31 March 2001. At the Pacific buoy locations, individual swell events were identified in the spectra from the three models and the buoy data. Predicted and observed swell frequencies and arrival directions are compared as well as the total energy transported past the buoy over the duration of each individual event. At all buoy locations, predicted and observed wave energy fluxes integrated over fixed frequency ranges are compared. All three models yield reliable nowcasts of swell arrivals at the buoy locations. In most cases, the models under-predict the energy measured by the buoys. WAVEWATCH III better resolves low-frequency swells than WAM, possibly owing to a superior numerical scheme. Swell predictions at NCEP forced with AVN winds are more accurate than those at FNMOC forced with NOGAPS winds.
机译:在美国的两个预报中心,舰队数值气象和海洋学中心以及国家环境预报中心产生的全球海浪预报都通过频谱浮标测量进行了评估。在这项研究中,使用来自大西洋和太平洋国家数据浮标中心运营的3米铁饼和6米游牧浮标的数据,对运营中心的WAM和WAVEWATCH III预测的频率方向频谱的保真度进行了研究。斯克里普斯海洋学沿海数据信息计划研究所在加利福尼亚海岸沿线部署了Datawell定向Waverider浮标。比较中仅使用位于深水中的浮标。在2000年10月1日至2001年3月31日的六个月期间内,将频谱和平均波方向的模型现时预报与浮标测量结果进行了比较。在太平洋浮标位置,从三个模型和浮标的频谱中识别出了单独的膨胀事件。数据。比较预测和观察到的膨胀频率和到达方向,以及每个事件持续时间内通过浮标的总能量。在所有浮标位置,比较在固定频率范围内积分的预测和观察到的波能通量。这三种模型都可以可靠地预测浮标位置上涌浪的临近。在大多数情况下,模型会低估浮标所测得的能量。与WAM相比,WAVEWATCH III可以更好地解决低频波动问题,这可能是由于采用了出色的数值方案。在使用AVN风的NCEP下的膨胀预测要比使用NOGAPS风的FNMOC上的膨胀预测更为准确。

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    Wingeart Karen M.;

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