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Generation of transient waves by impulsive disturbances in an inviscid fluid with an ice-cover

机译:带有冰盖的不粘流体中的脉冲干扰产生的瞬变波

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The dynamic responses of an ice-covered fluid to impulsive disturbances are analytically investigated for two- and three-dimensional cases. The initially quiescent fluid of infinite depth is assumed to be inviscid, incompressible and homogenous. The thin ice-cover is modelled as a homogenous elastic plate with negligible inertia. Four types of impulsive concentrated disturbances are considered, namely an instantaneous mass source immersed in the fluid, an instantaneously dynamic load on the plate, an initial impulse on the surface of the fluid, and an initial displacement of the ice plate. The linearized initial-boundary-value problem is formulated within the framework of potential flow. The solutions in integral form for the vertical deflexions at the ice-water interface are obtained by means of a joint Laplace-Fourier transform. The asymptotic representations of the wave motions for large time with a fixed distance-to-time ratio are derived by making use of the method of stationary phase. It is found that there exists a minimal group velocity and the wave system observed depends on the moving speed of the observer. For an observer moving with the speed larger than the minimal group velocity, there exist two trains of waves, namely the long gravity waves and the short flexural waves, the latter riding on the former. Moreover, the deflexions of the ice-plate for an observer moving with a speed near the minimal group velocity are expressed in terms of the Airy functions. The effects of the presence of an ice-cover on the resultant wave amplitudes, the wavelengths and periods are discussed in detail. The explicit expressions for the free-surface gravity waves can readily be recovered by the present results as the thickness of ice-plate tends to zero.
机译:对于二维和三维情况,研究了覆冰流体对脉冲干扰的动态响应。最初无限深的静态流体被假定为不粘稠,不可压缩且均质的。薄冰盖被建模为具有可忽略的惯性的均匀弹性板。考虑了四种类型的脉冲集中扰动,即浸没在流体中的瞬时质量源,板上的瞬时动态载荷,流体表面上的初始脉冲以及冰板的初始位移。线性化的初始边界值问题是在潜在流的框架内制定的。通过联合的Laplace-Fourier变换获得在冰水界面的垂直挠曲的整体形式的解。利用固定相位方法,推导了具有固定时空比的大时间波动的渐近表示。发现存在最小的群速度,并且观察到的波系统取决于观察者的移动速度。对于以大于最小群速度的速度移动的观察者,存在两列波,即长重力波和短弯曲波,后者位于前者之上。此外,以艾里函数来表示对于观察者以接近最小群速度的速度运动的冰板的挠度。详细讨论了冰盖的存在对合成波振幅,波长和周期的影响。当冰板厚度趋于零时,通过本发明的结果可以很容易地恢复出自由表面重力波的明确表达式。

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