在三维自由表面上,水以定涡量流动

Calin Iulian Martin
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引用次数: 3

摘要

本文综述了满足三维常涡量(不消失)水波问题的重力水流的最新研究结果。本文的主要目的是证明具有恒定不消失涡量的重力水流虽然满足三维水波方程,但具有二维特征。更准确地说,流动不会在两个水平方向中的任何一个方向上改变。通过旋转框架,并将地球物理效应(以科里奥利加速度的形式)引入控制方程,流的二维特征仍然存在。然而,流的二维现在在水平面上表现出来。在方程中加入向心项进一步简化了流动(在恒定涡量矢量的假设下):速度场消失了,但是,压力函数在水平和垂直变量中是二次多项式,并且,令人惊讶的是,表面是非平坦的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On three-dimensional free surface water flows with constant vorticity
We present a survey of recent results on gravity water flows satisfying the three-dimensional water wave problem with constant (non-vanishing) vorticity vector. The main focus is to show that a gravity water flow with constant non-vanishing vorticity has a two-dimensional character in spite of satisfying the three-dimensional water wave equations. More precisely, the flow does not change in one of the two horizontal directions. Passing to a rotating frame, and introducing thus geophysical effects (in the form of Coriolis acceleration) into the governing equations, the two-dimensional character of the flow remains in place. However, the two-dimensionality of the flow manifests now in a horizontal plane. Adding also centripetal terms into the equations further simplifies the flow (under the assumption of constant vorticity vector): the velocity field vanishes, but, however, the pressure function is a quadratic polynomial in the horizontal and vertical variables, and, surprisingly, the surface is non-flat.
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