Performance evaluation of WAVEWATCH III model in the Persian Gulf using different wind resources

被引:0
|
作者
Mohammad Hossein Kazeminezhad
Seyed Mostafa Siadatmousavi
机构
[1] Iranian National Institute for Oceanography and Atmospheric Science,Ocean Engineering and Technology Research Center
[2] Iran University of Science and Technology,School of Civil Engineering
来源
Ocean Dynamics | 2017年 / 67卷
关键词
Significant wave height; Shamal wind; Wave hindcast; Persian Gulf; CCMP; GFS; ECMWF; WAM cycle 4; Altimeter;
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中图分类号
学科分类号
摘要
The third-generation wave model, WAVEWATCH III, was employed to simulate bulk wave parameters in the Persian Gulf using three different wind sources: ERA-Interim, CCMP, and GFS-Analysis. Different formulations for whitecapping term and the energy transfer from wind to wave were used, namely the Tolman and Chalikov (J Phys Oceanogr 26:497–518, 1996), WAM cycle 4 (BJA and WAM4), and Ardhuin et al. (J Phys Oceanogr 40(9):1917–1941, 2010) (TEST405 and TEST451 parameterizations) source term packages. The obtained results from numerical simulations were compared to altimeter-derived significant wave heights and measured wave parameters at two stations in the northern part of the Persian Gulf through statistical indicators and the Taylor diagram. Comparison of the bulk wave parameters with measured values showed underestimation of wave height using all wind sources. However, the performance of the model was best when GFS-Analysis wind data were used. In general, when wind veering from southeast to northwest occurred, and wind speed was high during the rotation, the model underestimation of wave height was severe. Except for the Tolman and Chalikov (J Phys Oceanogr 26:497–518, 1996) source term package, which severely underestimated the bulk wave parameters during stormy condition, the performances of other formulations were practically similar. However, in terms of statistics, the Ardhuin et al. (J Phys Oceanogr 40(9):1917–1941, 2010) source terms with TEST405 parameterization were the most successful formulation in the Persian Gulf when compared to in situ and altimeter-derived observations.
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页码:839 / 855
页数:16
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