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Three-dimensional exponential asymptotics and Stokes surfaces for flows past a submerged point source

Published online by Cambridge University Press:  16 October 2024

Yyanis Johnson-Llambias
Affiliation:
Department of Mathematical Sciences, University of Bath, Bath BA2 7AY, UK
Philippe H. Trinh*
Affiliation:
Department of Mathematical Sciences, University of Bath, Bath BA2 7AY, UK
*
†Email address for correspondence: p.trinh@bath.ac.uk

Abstract

When studying two-dimensional fluid–body interactions in the low-Froude limit, traditional asymptotic theory predicts a waveless free surface at every order. The waves are, in fact, exponentially small and it has been well-established that such waves ‘switch on’ seemingly instantaneously across so-called Stokes lines, partitioning the fluid domain into wave-free regions and regions with waves. In three dimensions, the Stokes-line concept extends to higher-dimensional Stokes surfaces. This article is concerned with the archetypal problem of uniform flow over a point source, reminiscent of, but separate to, the famous Kelvin wave problem. In prior research, the intersection of the Stokes surface with the free surface was found, in implicit form, for this case of a point source. However, on account of the algebraic manipulations required, it is not clear how this approach can be extended to more challenging settings. Here we develop a numerical-based procedure that allows the Stokes surface to be computed. The intersections of the Stokes surfaces with both the free surface and the deeper fluid are discussed for the case of the point source. Crucially, this procedure provides an important tool for generalising exponential asymptotics to the case of nonlinear (non-point-source) wave-generating bodies.

Information

Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2024. Published by Cambridge University Press.
Figure 0

Figure 1.(a) A numerical surface wave calculated for $\epsilon = 0.15$. The underlying steady flow is in the positive $x$-direction. A point-source (indicated by a bold circle) is placed below the free surface (indicated by light grey shading). The interaction of this flow with the point-source induces a downstream wavetrain. The free surface is calculated by direct numerical integration of the Fourier integral in Appendix A. (b) Schematic of the wavetrain; note that transverse and divergent waves form a wavetrain similar to, but distinct, from that seen in the classic Kelvin-ship problem.

Figure 1

Figure 2.Contour plots of the singulant branches corresponding to the transverse waves, $\chi _{T1}$, and divergent waves, $\chi _{D1}$. This can be compared with figure 2 in Lustri & Chapman (2013). Visualisations of all eight singulant functions can be seen in Lustri (2012): (a) Re($\chi _{T1}$); (b) Im($\chi _{T1}$); (c) Re($\chi _{D1}$); (d) Im($\chi _{D1}$).

Figure 2

Figure 3.How rays with initial origin coordinate $s\in \mathbb {C}$ are used to construct the four (of eight) singulant functions, $\chi _{T1}$, $\chi _{T2}$, $\chi _{D1}$ and $\chi _{D2}$. (a) Complex rays are solved beginning from a point in $s\in \mathbb {C}$ with a choice of branch sign $(\mathrm {br}(y_0), \mathrm {br}(p_0))$. The eight patterned regions of the $s$-plane possess boundaries corresponding to those points $s\in \mathbb {C}$ where $1/x(s) \to 0$ and $1/y(s) \to 0$. (b) Rays intersect real $(x,y)$-space in one of eight configurations (four shown); finally (c) each branch of $\chi$ is found via the correspondence of quadrants labelled A1–4, B1–4, C1–4 and D1–4. Here, only four of the eight branches of $\chi$ are shown.

Figure 3

Figure 4.The ray-shooting procedure developed in Algorithm II, showing a collection of the random walks done in each of the eight regions of the $s$-plane, as illustrated in figure 3(a). The stepping length is taken with a default value of $\delta_{s} = 0.05$ and the maximum threshold $L = 5$. Each point is then used as the initial condition for the ray-shooting procedure. This corresponds to a source depth of $h = 1$.

Figure 4

Figure 5.Each ray initiated along the paths in figure 4 is solved to an intersection point in real $(x, y)$-space. The insets show the collected values of $(x, y, \chi )$ for (a) $\operatorname {Re}\chi$ and (b) $\operatorname {Im} \chi$. For clarity, only a selection of the branches are shown corresponding to the branch choice $(\mathrm {br}(y_0), \mathrm {br }(p_0)) = (+1, -1)$. These are to be compared with figure 4 quadrants A1–4 and B1–4. Within each quadrant of the $(x, y)$ plane, two Riemann sheets are visible; each sheet then coloured by one of the eight colours in figure 4. These are then associated to one of four branches of $\chi _{T1}$, $\chi _{T2}$, $\chi _{D1}$ and $\chi _{D2}$. Note that these must be combined with the rays with $(\mathrm {br} (y_0), \mathrm {br }(p_0)) = (-1; 1)$ to produce the complete Riemann sheet for each of the four singulants. These complex-ray solutions correspond to a source depth of $h = 1$.

Figure 5

Figure 6.A visualisation of the complex-ray procedures presented in §§ 5 and 8. The physical free surface is indicated by the horizontal plane with grey shading. When the solution at a given point is analytically continued we visualise this as an embedded plane ($\mathbb {R}^2$) or volume ($\mathbb {R}^3$) unfurling from the relevant point.

Figure 6

Figure 7.(a) As shown in the $(x, y, z)$-space, transverse-wave branches are switched on across the Stokes surface defined by $x=0$ separating regions $\boldsymbol {A}$ and $\boldsymbol {B}$ (not shown); also there is a switch-on of divergent waves across the second-generation Stokes surface (shown meshed), separating regions $\boldsymbol {B}$ and $\boldsymbol {C}$. The source is shown as a red star. The surface has been generated for a source depth of $h = 1$, but other choices produce similar images. In (b), a top-down view of the $(x, y)$ plane showing schematically that the wave field is composed of regions in which the solution, as $\epsilon \to 0$ in the low-Froude limit, has no waves ($\boldsymbol {A}$), transverse waves ($\boldsymbol {B}$) and both transverse and divergent waves ($\boldsymbol {C}$). The symbols $\oplus$ and $\otimes$ denote regions referred to in Appendix A. In (c), we plot the wave solution, computed from direct integration of the integral, as in figure 1.

Figure 7

Figure 8.Three contour plots corresponding to $\chi _{T1}$ at levels of $z = 0$, $z = -0.4$ and $z = -0.9$. For visual aid, we have also plotted the surface that intersects the level set $\chi _{T1} = 2.2$. The top contour level, shown in blue, corresponds to the free-surface visualisation as shown in figure 1, and placed slightly higher than $z = 0$ for clarity. This corresponds to a small source placed at a height of unit depth below the surface.

Figure 8

Figure 9.From top to bottom: a continuous deformation of the integration contour $[0,2{\rm \pi} ]$ into the path of steepest descent for a point in region $\boldsymbol {C}$, $(x,y,z)\approx (8.29,1.11,0)$ (cf. figure 7). The numerical data allowing the generation of these curves can be found in the supplementary data (Johnson-Llambias & Trinh 2024).

Figure 9

Figure 10.Equal phase contours (paths of steepest descent/ascent) for locations slightly left of, on, and slightly right of the second-generation Stokes line: (a) $(x,y)\approx (6.71, 0.89)\in \boldsymbol {B}$; (b) $(x,y)\approx (7.48, 0.99)$; (c) $(x,y)\approx (8.29, 1.11)\in \boldsymbol {C}$.