近岸大区域水波数学模型及其数值求解

从水波发展方程出发,导出了大区域缓坡水波数学模型,并采用交错网格系统下的有限差分法对该数学模型进行了数值求解,计算结果表明该数学模型在粗网格下也能得到与实验结果比较一致的结果,从而表明该模型可用于较大区域的水波问题.该模型具有编程简单、求解比较快速、经济的优点.     

结合抛物型缓坡方程计算波浪辐射应力

将波浪辐射应力与抛物型缓坡方程中的待求变量联系起来,提出了一种计算辐射应力的新方法,并用有限差分法对控制方程进行了数值求解。数值结果表明这种方法精度高、编程简单、求解快速,可用于实际大区域波浪辐射应力的计算。     

基于TM图像的潮滩表层沉积物含水量推算模型研究——以江苏辐射沙洲区为例

潮滩表层沉积物含水量是反映潮滩与潮水周期性作用并指示潮滩高程的重要指标,了解潮滩表层沉积物含水量是开发利用潮滩资源的重要工作之一。以江苏辐射沙洲为例,在对应于2000年4月的TM遥感图像成像时潮位特征的潮汐周期时,测量了两条断面的表层沉积物含水量,然后通过对辐射沙洲TM遥感图像的多种处理及其比较,找出了TM图像与潮滩表层沉积物含水量的相关系数绝对值最高的数字图像处理方法,然后再进行傅立叶变换等处理,并推算出可决系数较高的表层沉积物含水量推算模型。     

近岸海域波浪场中污染物运动的实验研究

通过实验模拟,研究了缓坡海岸带(坡度为1:100和1:40)波浪场中污染物的运动.给出了污染物在波浪破碎区和非破碎区运动范围的变化,讨论了在规则波和非规则波作用下波浪破碎区和非破碎区污染物运动的宏观变化趋势.     

Numerical Modeling of the Hyperbolic Mild-Slope Equation in Curvilinear Coordinates

The mild-slope equation is familiar to coastal engineers as it can effectively describe wave propagation in nearshore regions. However,its computational method in Cartesian coordinates often renders the model inaccurate in areas with irregular shorelines,such as estuaries and harbors. Based on the hyperbolic mild-slope equation in Cartesian coordinates,the numerical model in orthogonal curvilinear coordinates is developed. The transformed model is discretized by the finite difference method and solved by th...     

状态空间模型在海洋波能转换系统中的应用 Ⅱ.单个矩形振荡浮子装置运动受力分析的解析方法

对线性入射波作用下的矩形振荡浮子运动受力分析给出了一种新的解析方法.对该方法首先采用特征函数展开法得到绕射速度势的一种新解析式,然后直接由绕射势和入射势来计算波浪激励力.与经典方法相比可以看出,对于立面二维问题,由于绕射势和辐射势的计算量相当,因此该方法比过去常用的解析法更为简单.为了验证方法的正确性,采用该方法对过去文献介绍的经典算例进行了计算,得到了与过去方法完全一致的结果,从而证明该方法是正确的.     

淤泥质海岸形态的演变及形成机制

在淤长型和侵蚀型岸段之间,存在着一种由淤积到侵蚀的过渡型岸段。通过剖面测量、粒度分析和地质调查,认为过渡型岸段具有上部淤积下部冲刷、冲刷逐渐向上部扩展、潮滩表层沉积物不断租化、淤积带逐渐变窄最后过渡到全剖面侵蚀的基本特征和发展趋势。     

状态空间模型在海洋波能转换系统中的应用 Ⅰ.数值模拟方法改进

状态空间模型是研究海洋波能转换系统相互作用的一种有效数学模型.应用该模型的关键之一是如何根据实验或计算的脉冲响应函数来高效地确定状态空间模型中的矩阵参数.结合最优化理论中的单纯形法、最小二乘法以及矩阵指数的简化算法,提出了一种确定状态空间模型矩阵参数的有效数值方法.数值试验表明,由于该方法克服了高斯-牛顿方法的局部收敛性及其需求解矩阵指数关于参数的导数的缺点,因此大大扩展了初值的可选范围,有效地提高了数值模拟效率,并且使数值模拟结果具有较高精度.     

近岸波浪和波生流环境中泥沙输运的数值模拟

Owing to lack of observational data and accurate definition,it is difficult to distinguish the Kuroshio intrusion water from the Pacific Ocean into the South China Sea(SCS).By using a passive tracer to identify the Kuroshio water based on an observation-validated three-dimensional numerical model MITgcm,the spatio-temporal variation of the Kuroshio intrusion water into the SCS has been investigated.Our result shows the Kuroshio intrusion is of distinct seasonal variation in both horizontal and vertical directions.In winter,the intruding Kuroshio water reaches the farthest,almost occupying the area from 18°N to 23°N and 114°E to 121°E,with a small branch flowing towards the Taiwan Strait.The intrusion region of the Kuroshio water decreases with depth gradually.However,in summer,the Kuroshio water is confined to the east of 118°E without any branch reaching the Taiwan Strait;meanwhile the intrusion region of the Kuroshio water increases from the surface to the depth about 205 m,then it decreases with depth.The estimated annual mean of Kuroshio Intrusion Transport(KIT) via the Luzon Strait is westward to the SCS in an amount of –3.86×106 m3/s,which is larger than the annual mean of Luzon Strait Transport(LST) of –3.15×106 m3/s.The KIT above 250 m accounts for 60%–80% of the LST throughout the entire water column.By analyzing interannual variation of the Kuroshio intrusion from the year 2003 to 2012,we find that the Kuroshio branch flowing into the Taiwan Strait is the weaker in winter of La Ni?a years than those in El Ni?o and normal years,which may be attributed to the wind stress curl off the southeast China then.Furthermore,the KIT correlates the Ni?o 3.4 index from 2003 to 2012 with a correlation coefficient of 0.41,which is lower than that of the LST with the Ni?o 3.4 index,i.e.,0.78.     

用VOF方法模拟横流下窄缝紊动射流

采用标准双方程k-ε紊流模型和VOF方法建立二维数值模型,模拟有横流情况下底部排污问题.将回流区的分析结果与试验进行了对比,吻合较好.分别将速度和浓度轨迹线拟合成简单的表达式并与试验拟合作了比较.通过对速度和浓度场的分析得到一些有益的结论.