JONSWAP波环境下湍动射流三维大涡模拟研究

在σ坐标下,采用分步算法求解3维滤波后的N-S方程,其中亚格子模型采用作者提出的动力拟序涡粘性模型封闭。数值模拟了波动环境下湍动射流问题。其数值计算结果与实验值和理论值吻合良好。分析了JON-SWAP波环境下垂直湍动射流回流区域拟涡能分布特性以及JONSWAP波作用下射流掺混特性;给出了射流掺混图像和射流对JONSWAP波波能损耗影响特性。成果为随机波作用下污染物排放的掺混与稀释特性研究提供了手段与理论依据。

An Appropriate Unidirectional Wave Spectrum Model for the Strait of Hormuz

The objective of this paper is to introduce an appropriate unidirectional wave spectrum model for the Strait of Hormuz. The research is focused on assessing performance of standard wave spectrum models in the region. By evaluating such models based on valuable measurement data recently published, the calibration procedure has been conducted on such standard models to reach a better concordance between a modified standard spectral model and observed field spectra. The calibration is performed initially with respect to four distinct directions related to four available measurement stations. So, it results in four sets of coefficients for a nominated model. Next, it is continued to reach just one model insensitive to directions. Results clearly showed that the International Towing Tank Conference （ITTC） model is more appropriate than Joint North Sea Wave Project （JONSWAP） and Pierson and Moskowitz （PM） models in this area, even without any calibration. However, modifications have been successful on improving the conformity of the model.

基于Gerstner函数和JONSWAP海浪谱的海浪仿真

针对单一海浪仿真方法在不同场景应用的局限性,提出了基于Gerstner函数与JONSWAP海浪谱相结合的海浪仿真方法,实现了不同波浪强度下的海浪建模.选取了Gerstner函数方程组作来海浪构造模型,并将其扩展成三维形式模拟海浪的细节和真实度;为了控制海浪模型并实现海浪的随机性、多变性、真实性,采用了JONSWAP海浪谱获取控制海浪模型的参数,进而建立了海浪仿真模型;针对多组海浪谱的频谱参数进行海浪仿真和不同海浪建模方法的海浪仿真,实验结果表明,所提方法有效性和实用性较好,真实度高,并适用于多种海浪场景.

Large eddy simulation of vertical turbulent jets under JONSWAP waves

The effect of random waves on vertical plane turbulent jets is studied numerically and the mechanism behind the interaction of the jet and waves is analyzed. The large eddy simulation method is used and the σ-coordinate system is adopted. Turbulence is modeled by a dynamic coherent eddy model. The σ-coordinate transformation is introduced to map the irregular physical domain with a wavy free surface and an uneven bottom onto a regular computational domain. The fractional step method is used to solve the filtered Navier–Stokes equations. Results presented include the distribution of velocity, the decay law of the mean velocity along the jet axis, self-similar characteristics and volume flux per unit width. In particular, the role of coherent structures on the momentum transfer along the jet centerline and the jet instantaneous characteristics in JONSWAP waves are a special focus of this research. The numerical results obtained are of great theoretical importance in understanding the behavior of turbulent jets in random wave environments.

Wave Spectral Patterns during a Historical Cyclone: A Numerical Model for Cyclone Gonu in the Northern Oman Sea

The third generation wind-wave model Mike21-SW was used to study spectral characteristics of waves generated by the historical Cyclone Gonu in June 2007 along and off the Iranian coasts on the northern Oman Sea. The model was forced with the cyclone wind field generated using a Holland (1980) model based on cyclone data obtained from the Joint Typhon Warning Center (JTWC). The wave model was calibrated for the northern Oman Sea using bulk and spectral wave data at a station out of the Chabahar Bay. Evolution of directional-frequency spectra during the cyclone was investigated for two locations near the entrance and off the Chabahar Bay. At the offshore station, energy was contributed to the spectrum over an approximately 180 degree directional span that included different local and remotely generated waves. As the cyclone proceeded northwestward, all spectral directions continuously rotated in the clockwise direction at both locations. Frequency spectra at these locations were investigated for four different times corresponding to different locations of Cyclone’s eye and were justified using the sea growth parameter of the Joint North Sea Wave Project (JONSWAP) experiment. Using the modified JONSWAP parameters for hurricane conditions resulted in a frequency spectrum consistent with simulation results.

Numerical simulation and inversion of offshore area depth based on x-band microwave radar

A detection method of offshore area depth utilizing the x-band microwave radar is proposed. The method is based on the sea clutter imaging mechanism of microwave radar, and combined with dispersion equation of the liner wave theorem and least square method （LSM）, consequently get the inversion results of water depth in the detected region. The wave monitoring system OSMAR-X exploited by the Ocean State Laborato-ry, Wuhan University, based on a microwave radar has proven to be a powerful tool to monitor ocean waves in time and space. Numerical simulation and inversion of offshore area depth are carried out here; since JONSWAP model can give description of stormy waves in different growth phase, it is suitable for simulation. Besides, some results from measured data detected by OSMAR-X x-band radar located at Longhai of Fujian Province, China, validates this method. The tendency of the average water depths inferred from the radar images is in good agreement with the tide level detected by Xiamen tide station. These promising results suggest the possibility of using OSMAR-X to monitor operationally morphodynamics in coastal zones. This method can be applied to both shore-based and shipborne x-band microwave radar.

南海风浪条件下Spar式浮式风机平台的构型及参数

使用WAMIT软件建立OC3-Hywind Spar式浮式风机模型,联合FAST软件计算浮式风机在不同工况下的幅值响应算子;结合为南海海域波浪条件优化后的JONSWAP谱,对浮式风机进行不同工况下的响应谱分析及最大响应值计算,进一步阐述浮式平台结构构型参数的变化对整体结构在南海相应工况下的运动影响。

理论风浪谱修正方法及数值验证

为了研究特定海域范围内海浪的内部能量相对于频率的分布规律,本文以目标岛屿处"波浪骑士"式浮标提供的实际观测资料为依据,提出了一种基于实测资料的风浪数据筛选和理论风浪谱修正方法。通过讨论实测频谱与理论频谱的谱峰位置关系筛选出研究针对的风浪数据点,将实测风浪频谱与理论频谱进行对比分析,进而提出理论风浪谱的修正方法,并以增加参数的JONSWAP谱为靶谱对实测风浪数据进行拟合,得到了可以表达目标岛屿处风浪内部能量的理论谱形式,并进行了对比验证。研究结果表明:所提出的理论风浪谱修正方法,能够有效地筛选出实测数据集中的风浪数据,并完成对特定海域处风浪频谱的描述表达。

波列在时、空域的数值模拟试验及波要素的统计比较

利用Longuet-Higgins波浪模型,分别用无因次JONSWAP谱和文圣常谱生成时间序列的表面波列与其相匹配的空间序列表面波列,作波浪特征波要素间关系的数值试验检验。由实测资料核对表明,以往有关工程上应用的理论和经验关系有的可信度高,有的似应作改进,特别不能将在时间序列上得到的有关经验数据贸然用在空间序列的表面波上。