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• 图形学与可视化 • 上一篇    下一篇

海浪实时绘制中波浪谱的选择

摘 要:Phillips 谱是海浪实时绘制中常用的波浪谱。首先分析了Phillips 谱的结构,#br# 指出该谱是一个瞬时空间谱,其频率谱符合Neumann 形式,与P-M 谱接近,其方向分布函#br# 数为国际拖曳水池会议推荐的形式。令P-M 谱与Phillips 谱具有相同的单位面积波能,给出#br# 了Phillips 谱风速的确切含义并计算出该谱的常数。除了使用Phillips 谱,还尝试其它形式#br# 的谱。用P-M 谱和cos-2s 形式方向分布函数构造了瞬时空间谱PM-cos2s 形式,用JONSWAP#br# 谱和Poisson 形式方向分布函数构造了瞬时空间谱J-Po 形式。比较3 种谱的绘制结果发现,#br# 使用Phillips 谱、PM-cos2s 谱的绘制结果均能反映风速对海浪的影响,不能反映风距的影响,#br# 使用J-Po 谱的绘制结果既能反映风速、也能反映风距对海浪的影响,且三者的绘制帧率一#br# 致。如果要选择适合航海模拟器中海浪绘制的瞬时空间谱,该谱的风参数既应包括风速,也#br# 应包括风距,且生成波应在风向的(-?,?]范围内,因此J-Po 谱在三者中最适合航海模拟器。#br# 绘制结果已应用于航海模拟器中。#br# 关 键 词:海浪绘制;Phillips 波浪谱;方向分布函数;风速   

  • 出版日期:2015-04-30 发布日期:2015-03-30

On Selection of the Wave Spectrum in Ocean Wave Real-time Rendering

Abstract: The Phillips spectrum is widely used in ocean wave real-time rendering. First, the#br# structure of the spectrum is analyzed. The Phillips spectrum is an instantaneous spatial spectrum.#br# Its frequency spectrum is in accord with the spectrum form raised by Neumann and similar to the#br# P-M spectrum. Its directional distribution function is that recommended by the international#br# towing tank conference. On the hypothesis that the wave energy per unit area of the Phillips#br# spectrum equals that of the P-M spectrum, the spectral constant is computed, and the spectral wind#br# speed is clarified. In addition to the Phillips spectrum, other spectra are tried as well. The P-M#br# spectrum and the directional distribution function of cos-2s form are used to construct an#br# instantaneous spatial spectrum, denoted as PM-cos2s form, and the JONSWAP spectrum and the#br# direction distribution function of Poisson form are applied for constructing an instantaneous#br# spatial spectrum, denoted as J-Po from. The comparison of the rendering results of the three#br# spectra shows that the wave rendered with the Phillips spectrum and PM-cos2s spectrum can#br# reflect wind speed influence on the wave, but cannot embody the fetch length influence, while the#br# wave rendered with J-Po spectrum can show the fetch length effect along with wind speed on the wave. With the same computer hardware, the frame rates of the three spectra are equal. For wave#br# rendering in the nautical simulator, the wind parameter of the selected spectrum should contain the#br# wind speed as well as fetch length, and the generated wave of the spectrum should distribute in#br# (-?,?] of the wind speed. So J-Po spectrum is more suitable than the other two for the nautical#br# simulator. The method was used in the nautical simulator.#br# Key words: ocean wave rendering; Phillips spectrum; directional distribution function; wind#br# speed   

  • Online:2015-04-30 Published:2015-03-30

摘要: Phillips 谱是海浪实时绘制中常用的波浪谱。首先分析了Phillips 谱的结构,
指出该谱是一个瞬时空间谱,其频率谱符合Neumann 形式,与P-M 谱接近,其方向分布函
数为国际拖曳水池会议推荐的形式。令P-M 谱与Phillips 谱具有相同的单位面积波能,给出
了Phillips 谱风速的确切含义并计算出该谱的常数。除了使用Phillips 谱,还尝试其它形式
的谱。用P-M 谱和cos-2s 形式方向分布函数构造了瞬时空间谱PM-cos2s 形式,用JONSWAP
谱和Poisson 形式方向分布函数构造了瞬时空间谱J-Po 形式。比较3 种谱的绘制结果发现,
使用Phillips 谱、PM-cos2s 谱的绘制结果均能反映风速对海浪的影响,不能反映风距的影响,
使用J-Po 谱的绘制结果既能反映风速、也能反映风距对海浪的影响,且三者的绘制帧率一
致。如果要选择适合航海模拟器中海浪绘制的瞬时空间谱,该谱的风参数既应包括风速,也
应包括风距,且生成波应在风向的(-,]范围内,因此J-Po 谱在三者中最适合航海模拟器。
绘制结果已应用于航海模拟器中。

关键词: 海浪绘制, Phillips 波浪谱, 方向分布函数, 风速

Abstract: The Phillips spectrum is widely used in ocean wave real-time rendering. First, the
structure of the spectrum is analyzed. The Phillips spectrum is an instantaneous spatial spectrum.
Its frequency spectrum is in accord with the spectrum form raised by Neumann and similar to the
P-M spectrum. Its directional distribution function is that recommended by the international
towing tank conference. On the hypothesis that the wave energy per unit area of the Phillips
spectrum equals that of the P-M spectrum, the spectral constant is computed, and the spectral wind
speed is clarified. In addition to the Phillips spectrum, other spectra are tried as well. The P-M
spectrum and the directional distribution function of cos-2s form are used to construct an
instantaneous spatial spectrum, denoted as PM-cos2s form, and the JONSWAP spectrum and the
direction distribution function of Poisson form are applied for constructing an instantaneous
spatial spectrum, denoted as J-Po from. The comparison of the rendering results of the three
spectra shows that the wave rendered with the Phillips spectrum and PM-cos2s spectrum can
reflect wind speed influence on the wave, but cannot embody the fetch length influence, while the
wave rendered with J-Po spectrum can show the fetch length effect along with wind speed on the wave. With the same computer hardware, the frame rates of the three spectra are equal. For wave
rendering in the nautical simulator, the wind parameter of the selected spectrum should contain the
wind speed as well as fetch length, and the generated wave of the spectrum should distribute in
(-,] of the wind speed. So J-Po spectrum is more suitable than the other two for the nautical
simulator. The method was used in the nautical simulator.

Key words: ocean wave rendering, Phillips spectrum, directional distribution function, wind
speed