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INTERACTION OF WATER GRAVITY WAVES WITH ELASTIC ICE FLOES

机译:水重力波与弹性冰层的相互作用

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摘要

The self-consistence motion of a fluid and elastically oscillating plates partially covering fluid is simulated numerically. The problem is reduced to simulation solution of the Laplace equation for the fluid and equation of elastic plate oscillations for ice motion. The numerical and analytical solutions, obtained using an integral equation containing the Green function, are compared. In order to solve the problem numerically the boundary elements method for the Laplace equation and the finite element method for the equation describing the elastic plate motion are proposed. The coefficients of surface gravity wave transmission and reflection from the floating plate are estimated. It is shown that the solution can be presented as quasi-periodic one with characteristics determined by the initial value of the wave and ice foe parameters. The ice floe exert a filtering effect on the surface wave spectrum, essentially reducing its most deflectable components.
机译:数值模拟了流体和部分覆盖流体的弹性振动板的自保持运动。问题被简化为流体的拉普拉斯方程和冰运动的弹性板振动方程的模拟解。比较了使用包含格林函数的积分方程获得的数值和解析解。为了从数值上解决这个问题,提出了描述拉普拉斯方程的边界元方法和描述弹性板运动的方程的有限元方法。估算了表面重力波在浮板上的透射和反射系数。结果表明,该解可以表示为准周期解,其特征由波浪和冰敌参数的初始值确定。浮冰在表面波谱上发挥过滤作用,从根本上减少了其最易偏转的成分。

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