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Computation of three-dimensional flexural-gravity solitary waves in arbitrary depth

机译:在任意深度中计算三维弯曲 - 重力孤立波

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Fully-localised solitary waves propagating on the surface of a three-dimensional ideal fluid of arbitrary depth, and bounded above by an elastic sheet that resists flexing, are computed. The cases of shallow and deep water are distinct. In shallow water, weakly nonlinear modulational analysis (see Milewski & Wang6) predicts waves of arbitrarily small amplitude and these are found numerically. In deep water, the same analysis rules out the existence of solitary waves bifurcating from linear waves, but, nevertheless, we find them at finite amplitude. This is accomplished using a continuation method following the branch from the shallow regime. All solutions are computed via a fifth-order Hamiltonian truncation of the full ideal free-boundary fluid equations. We show that this truncation is quantitatively accurate by comparisons with full potential flow in two-dimensions.
机译:计算在任意深度的三维理想流体的表面上传播的完全局部孤立波,并通过抵抗弯曲的弹性片材界定。浅水和深水的病例是截然不同的。在浅水中,弱非线性调制分析(参见Milewski&Wang6)预测任意小幅度的波浪,这些都在数值上发现。在深水中,相同的分析规定了从线性波分叉分叉的孤立波的存在,但是,我们在有限幅度下找到它们。这是使用浅水区分支后的延续方法完成的。通过全理想自由边界流体方程的第五次汉密尔顿截断所有解决方案。我们表明,通过对两维的全电流的比较,这种截断是定量准确的。

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