Based on the simulation with SWAN wave model and data of ERA-Interim from 1979 to 2016, how the waves propagate globally and why swell pools distribute in the eastern ocean were investigated in this study. The simulat...Based on the simulation with SWAN wave model and data of ERA-Interim from 1979 to 2016, how the waves propagate globally and why swell pools distribute in the eastern ocean were investigated in this study. The simulation results show that waves from North Pacific and North Atlantic mainly propagate southeastward or southward and swells generated in Southern Ocean spread northeastward. The waves from high latitude regions spread along the east coast and encounter in the tropical Pacific and Atlantic to form swell fronts around equator and then turn eastward. As the weak wind field with numerous swell inflows, swell pools are gener- ally located on the eastern side of the ocean basin, where the swell index S are greater than 0.9 calculated using ERA-20C data for the period of 1981 2010. Another remarkable feature is that swell pools move southward and split into two parts in winter, while they move northward and merge together in summer.展开更多
There exists a tongue-shaped swell-dominance pool known as Swell Pool（SP） in the Eastern Pacific region.The monthly-mean wave transports（WT） for each month of 2000 is computed using the wave products of ECMWF rean...There exists a tongue-shaped swell-dominance pool known as Swell Pool（SP） in the Eastern Pacific region.The monthly-mean wave transports（WT） for each month of 2000 is computed using the wave products of ECMWF reanalysis data.By comparing the 2000 monthly-mean WT and monthly-mean wind field from QUICKSCAT,large differences are found between the wave transport direction and the wind direction over the Eastern Pacific.This may serve as an evidence for the existence of the SP in this region.The work done in this study indicates that the sources of swell in the Tropical Eastern Pacific（TEP） are in the westerly regions of the Southern and Northern Pacific.展开更多
In order to consider the viscous effect,the introduction of a parametric dissipation and new results are realized by applying the new formulation combining and dynamic conditions over the free-surface with viscous ter...In order to consider the viscous effect,the introduction of a parametric dissipation and new results are realized by applying the new formulation combining and dynamic conditions over the free-surface with viscous terms. The dispersion equation is then modified by assuming an additional term in the boundary condition at the free-surface and wave-number becomes complex number with a small imaginary part which ensures the decay of wave amplitudes. The comparisons of numerical results and model test measurement on wave elevation at the moon-pool center is obtained both for the peak period and for the amplitude at resonance by choosing an appropriated dissipation coefficient. The results show that the introduce dissipation is not only effective but also reliable to provide realistic predictions.展开更多
基于CFD(Computational Fluid Dynamics)和粘性数值波浪水池技术,对顺浪航态的规则波波浪环境进行数值模拟,采用边界造波法进行波浪生成,VOF(Volume of Fluid)法模拟自由面。本文改进了传统的基于规则波的顶浪数值模拟方法,在特定波浪...基于CFD(Computational Fluid Dynamics)和粘性数值波浪水池技术,对顺浪航态的规则波波浪环境进行数值模拟,采用边界造波法进行波浪生成,VOF(Volume of Fluid)法模拟自由面。本文改进了传统的基于规则波的顶浪数值模拟方法,在特定波浪、不同航速条件下进行了顺浪航态的数值水池模拟。根据模拟呈现的动态效果,以及与Matlab仿真结果的对比,对试验的准确性进行验证。展开更多
基金financially supported by the Public Science and Technology Research Funds Projects of Ocean (No. 201505007)the National Natural Science Foundation of China (NSFC) (No. 41276015)+2 种基金the Joint Project for the National Oceanographic Center by the NSFC and Shandong Government (No. U1406401)the Doctoral Fund of Ministry of Education of China (No. 20120132110004)the Hebei Agricultural University research project for talented scholars (No. YJ201835)
文摘Based on the simulation with SWAN wave model and data of ERA-Interim from 1979 to 2016, how the waves propagate globally and why swell pools distribute in the eastern ocean were investigated in this study. The simulation results show that waves from North Pacific and North Atlantic mainly propagate southeastward or southward and swells generated in Southern Ocean spread northeastward. The waves from high latitude regions spread along the east coast and encounter in the tropical Pacific and Atlantic to form swell fronts around equator and then turn eastward. As the weak wind field with numerous swell inflows, swell pools are gener- ally located on the eastern side of the ocean basin, where the swell index S are greater than 0.9 calculated using ERA-20C data for the period of 1981 2010. Another remarkable feature is that swell pools move southward and split into two parts in winter, while they move northward and merge together in summer.
基金The National Basic Research Programof China under contract Nos 2005CB422302,2005CB422307 and 2007CB411806the Nation-al Natural Science Foundation of China under contract No. 40490263
文摘There exists a tongue-shaped swell-dominance pool known as Swell Pool（SP） in the Eastern Pacific region.The monthly-mean wave transports（WT） for each month of 2000 is computed using the wave products of ECMWF reanalysis data.By comparing the 2000 monthly-mean WT and monthly-mean wind field from QUICKSCAT,large differences are found between the wave transport direction and the wind direction over the Eastern Pacific.This may serve as an evidence for the existence of the SP in this region.The work done in this study indicates that the sources of swell in the Tropical Eastern Pacific（TEP） are in the westerly regions of the Southern and Northern Pacific.
基金Sponsored by the National Natural Science Foundation of China(Grant No.51079032)
文摘In order to consider the viscous effect,the introduction of a parametric dissipation and new results are realized by applying the new formulation combining and dynamic conditions over the free-surface with viscous terms. The dispersion equation is then modified by assuming an additional term in the boundary condition at the free-surface and wave-number becomes complex number with a small imaginary part which ensures the decay of wave amplitudes. The comparisons of numerical results and model test measurement on wave elevation at the moon-pool center is obtained both for the peak period and for the amplitude at resonance by choosing an appropriated dissipation coefficient. The results show that the introduce dissipation is not only effective but also reliable to provide realistic predictions.
文摘基于CFD(Computational Fluid Dynamics)和粘性数值波浪水池技术,对顺浪航态的规则波波浪环境进行数值模拟,采用边界造波法进行波浪生成,VOF(Volume of Fluid)法模拟自由面。本文改进了传统的基于规则波的顶浪数值模拟方法,在特定波浪、不同航速条件下进行了顺浪航态的数值水池模拟。根据模拟呈现的动态效果,以及与Matlab仿真结果的对比,对试验的准确性进行验证。
