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在密度线性分布的分层流试验水槽中,对贴近侧壁面的半球体模型运动生成的内波进行了实验研究. 采用多通道电导率阵列,测量分析了拖曳模型产生内波的波形结构、垂向位移场及其相关速度等. 实验结果表明:半球体模型产生的内波可以分为两类,一类是由定常源激发的体积效应内波,另一类是由非定常源激发的尾迹内波,由前者转换为后者的临界内Froude(Fr)数是Frs =1.6;与球体模型实验比较,Frs约为球体的2/3,转换更迅速,界线更清
关键词:
分层流
半球模型
内波
尾迹 相似文献
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IntroductionItis known thatthere exists a special kind of solitary waves—the algebraic solitary waveas the disturbance range is close to the scale of vertical variation of density in thecontinuously stratified fluid.The algebraic solitary wave is governe… 相似文献
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A theoretical model for interaction of a submerged moving body with the conjugate flow in a three-layer fluid is proposed to depict the internal flat solitary wave, which is observed in experiments conducted by the present authors. A set of coupled nonlinear algebraic equations is derived for the interracial displacements. The numerical results indicate that (a) the conjugate flow due to a two-dimensional body moving at the bottom possesses an apparent behaviour with two convex interfaces, (b) the solution satisfying the existence criterion is always unique near the relatively stable state of system. Theoretical analysis is qualitatively consistent with the experimental results obtained. 相似文献
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