WAVEWATCH Ⅲ第三代海浪数值模式在中国东海的应用和改进Application and Improvement of Wavewatch Ⅲ Third Generation Wave Numerical Model in the East China Sea
曹赛超,高志一,赵栋梁
摘要(Abstract):
利用东海的浮标观测数据,比较了WAVEWATCHⅢ第三代海浪数值模式的ST2、ST4和ST6三种源函数方案在东海的适用性。结果表明,三种源函数方案在波高小于3 m中低风速情形下,模拟波高与观测波高符合的很好,而在波高大于3 m的高风速情形下,模拟波高偏大。在此基础上,提出了以波龄和波陡为参数的海面粗糙度参数化公式,以此来计算拖曳系数。该方案可以自动满足拖曳系数在临界风速达到饱和的观测事实,将上述拖曳系数计算方案应用于最新的ST6源函数方案,在保持中低风速时的模拟精度的同时,可有效地改善高风速时模拟波高偏大问题,而且可使模拟周期与浮标观测结果更为一致。
关键词(KeyWords): 海浪数值模式;源函数方案;拖曳系数;波龄;波陡
基金项目(Foundation): 国家自然科学基金项目(41876010)资助~~
作者(Author): 曹赛超,高志一,赵栋梁
DOI: 10.16441/j.cnki.hdxb.20220118
参考文献(References):
- [1] WAMDI Group.The WAM model—a third generation ocean wave prediction model[J].Journal of Physical Oceanography,1988,18:1775-1810.
- [2] Tolman H L.A third-generation model for wind waves on slowly varying,unsteady,and inhomogeneous depths and currents[J].Journal of Physical Oceanography,1991,21(6):782-797.
- [3] Tolman H L.Effects of numerics on the physics in a third-generation wind-wave model[J].Journal of Physical Oceanography,1992,22(10):1095-1111.
- [4] Tolman H L.User Manual and System Documentation of WAVEWATCH Ⅲ Version 1.18[R].Washington DC:National Oceanic and Atmospheric Administration,1999:110.
- [5] Stopa J,Ardhuin F,Babanin A,et al.Comparison and validation of physical wave parameterizations in spectral wave models[J].Ocean Modelling,2016,103:2-17.
- [6] Liu Q,Babanin A V,Fan Y,et al.Numerical simulations of ocean surface waves under hurricane conditions:Assessment of existing model performance[J].Ocean Modelling,2017,118:73-93,https://doi.org/10.1016/j.ocemod.2017.08.005.
- [7] 吴萌萌,王毅,万莉颖,等.WAVEWATCH Ⅲ模式在全球海域的数值模拟试验及结果分析[J].海洋预报,2016,33(5):31-40.Wu M,Wang Y,Wan L,et al.Numerical simulation test and result analysis of WAVEWATCH Ⅲ model in global waters[J].Ocean Forecast,2016,33(5):31-40.
- [8] 李明悝,侯一筠.利用QuikSCAT/NCE混合风场及WAVEWATCH模拟东中国海风浪场[J].海洋科学,2005,29(6):9-12.Li M,Hou Y.QuikSCAT /NCE mixed wind field and WAVEWATCH are used to simulate the wind and wave field in the East China Sea[J].Marine Science,2005,29(6):9-12.
- [9] 徐艳清.东中国海海浪数值模拟及波候统计分析[D].北京:中国科学院研究生院,2005.Xu Y.Numerical Simulation and Statistical Analysis of Wave Climate in the East China Sea[D].Beijing:Graduate School of Chinese Academy of Sciences,2005.
- [10] Saha S,Moorthi S,Wu X,et al.The NCEP climate forecast system version 2[J].Journal of Climate,2014,27(6):2185-2208.
- [11] Tolman H L,Chalikov D.Source terms in a third-generation wind wave model[J].Journal of Physical Oceanography,1996,26:2497-2518.
- [12] Ardhuin F,Chapron B,Collard F.Observation of swell dissipation across oceans[J].Geophysical Research Letters,2009,36,L06607,doi:10.1029/2008GL037030.
- [13] Ardhuin F,Rogers E,Babanin A,et al.Semiempirical dissipation source functions for ocean waves,Part Ⅰ,definition,calibration and validation[J].Journal of Physical Oceanography,2010,40(9):1917-1941.
- [14] Donelan M A,Babanin A V,Young I R,et al.Wave-follower field measurements of the wind-input spectral function.Part Ⅱ:Parameterization of the wind input[J].Journal of Physical Oceanography,2006,36:1672-1689.
- [15] Babanin A V.Breaking and Dissipation of Ocean Surface Waves[M].Cambridge:Cambridge University Press,2011:480.
- [16] Rogers W E,Babanin A V,Wang D W.Observation consistent input and whitecapping dissipation in a model for wind-generated surface waves:Description and simple calculations[J].Journal of Atmospheric and Oceanic Technology,2012,29:1329-1346.
- [17] Zieger S,Babanin A V,Rogers W E,et al.Observation based source terms in the third-generation wave model WAVEWATCH[J].Ocean Modelling,2015,96:2-25.
- [18] Liu Q,Rogers W E,Babanin A V,et al.Observation-based source terms in the third-generation wave model WAVEWATCH Ⅲ:Updates and verification[J].Journal of Physical Oceanography,2019,49:489-517.
- [19] Powell M D,Vickery P J,Reinhold T A.Reduced drag coefficient for high wind speeds in tropical cyclones[J].Nature,2003,422:279-283.
- [20] Hwang P A.A note on the ocean surface roughness spectrum[J].Journal of Atmospheric and Oceanic Technology,2011,28(3):436-443.doi:10.1175/2010JTECHO812.1.
- [21] Taylor,Karl E.Summarizing multiple aspects of model performance in a single diagram[J].Journal of Geophysical Research Atmospheres,2001,106(D7):7183-7192.
- [22] Chiang T L,Wu C R,Oey L Y.Typhoon Kai-Tak:An ocean’s perfect storm[J].Journal of Physical Oceanography,2011,41:221-233.
- [23] Sanford T B,Price J F,Girton J B,et al.Highly resolved observations and simulations of the ocean response to a hurricane[J].Geophysical Research Letters,2007,34:L13604.
- [24] Zhao D,Li M.Dependence of wind stress across an air-sea interface on wave states[J].Journal of Oceanography,2019,75(3):207-223.
- [25] Takagaki N,Komori S,Suzuki N,et al.Strong correlation between the drag coefficient and the shape of the wind sea spectrum over a broad range of wind speeds[J].Geophysical Research Letters,2012,39:L23604.
- [26] Zijlema M,Vledder G,Holthuijsen L.Bottom friction and wind drag for wave models[J].Coastal Engineering,2012,65:19-26.
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