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Calibration and skill assessment of two input and dissipation parameterizations in WAVEWATCH-Ⅲ model forced with ERA5 winds with application to Persian Gulf and Gulf of Oman

机译:校准和技能评估Wavatch-Ⅲ模型中的两种输入和耗散参数,用ErA5风与阿曼斯普尔夫和阿曼湾的应用

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The wind energy input and whitecap dissipation terms in the third generation wave models have been improved over the time. In this research, the well-known WAM-Cycle4, known as ST3, and the newest ST6 package in WAVEWATCH-III model were employed combined with ERAS wind data over the Persian Gulf and Gulf of Oman. In order to model the wave height appropriately over the study area in comparison with both in-situ and satellite observations, new combined error parameters were introduced leading to two major calibration values: (1) the local calibration values relating to either Persian Gulf (PGc) or Gulf of Oman (GOc); (2) the global calibration values over the entire computational domain (PGGOc). Considerably different model performance was appeared in the Persian Gulf (PG) compared to either the Gulf of Oman (GO) or entire computational domain (PGGO) when ST3 package was employed, while obtained results using ST6 package showed negligible sensitivity to the domain. Both ST3 and ST6 packages with default tuning values significantly underestimated the wave height and peak period in PG; however, slight underestimation (-0.03 m) for wave height and overestimation (-0.1 s) for mean wave period were obtained in GO. During the time period the cyclone Phet has traversed across the study area, the model overestimated the wave height in comparison with altimeter dataset. Mean bias distribution over the study area indicates that calibrated ST6 outperforms calibrated ST3 over GO; however, both packages provide similar results over PG. Considering different methods for nonlinear interaction term led to similar directional wave spectrums over the study area and negligible changes in bulk wave parameters.
机译:第三代波模型中的风能输入和白斑耗散术语已随时间提高。在本研究中,使用众所周知的WAM-Cycle4,称为ST3,以及Wavewatch-III模型中最新的ST6封装,并与Seras风数据相结合,在波斯湾和阿曼的海湾。为了与原位和卫星观测相比适当地模拟研究区域,引入了新的组合误差参数,导致两个主要校准值:(1)与波斯湾(PGC相关)的本地校准值)或阿曼的海湾(GOC); (2)整个计算域上的全局校准值(PGGOC)。与采用ST3封装的OMAn(GO)或整个计算领域(PGGO)的海湾相比,波斯湾(PG)中出现了相当不同的模型性能,同时使用ST6封装获得的结果对该域表示可忽略不计的敏感性。具有默认调谐值的ST3和ST6封装都显着低估了PG的波浪高度和峰值时段;然而,在GO中获得了用于平均波期的波浪高度和高估计(-0.1秒)的轻微低估(-0.03μm)。在时间段期间,旋风Phet穿过研究区域,模型与高度计数据集相比,模型高估了波形高度。研究区域的平均偏置分布表明校准的ST6优于校准的ST3超出去;然而,两种包都提供了PG的类似结果。考虑到非线性交互项的不同方法导致研究区域的相似方向波谱和散装波参数的可忽略变化。

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