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Particle paths in nonlinear Schrödinger models in the presence of linear shear currents

Published online by Cambridge University Press:  18 September 2018

C. W. Curtis*
Affiliation:
Department of Mathematics and Statistics, San Diego State University, San Diego, CA 92182, USA
J. D. Carter
Affiliation:
Mathematics Department, Seattle University, Seattle, WA 98122, USA
H. Kalisch
Affiliation:
Department of Mathematics, University of Bergen, Bergen 5020, Norway
*
†Email address for correspondence: ccurtis@mail.sdsu.edu

Abstract

We investigate the effect of constant-vorticity background shear on the properties of wavetrains in deep water. Using the methodology of Fokas (A Unified Approach to Boundary Value Problems, 2008, SIAM), we derive a higher-order nonlinear Schrödinger equation in the presence of shear and surface tension. We show that the presence of shear induces a strong coupling between the carrier wave and the mean-surface displacement. The effects of the background shear on the modulational instability of plane waves is also studied, where it is shown that shear can suppress instability, although not for all carrier wavelengths in the presence of surface tension. These results expand upon the findings of Thomas et al. (Phys. Fluids, vol. 24 (12), 2012, 127102). Using a modification of the generalized Lagrangian mean theory in Andrews & McIntyre (J. Fluid Mech., vol. 89, 1978, pp. 609–646) and approximate formulas for the velocity field in the fluid column, explicit, asymptotic approximations for the Lagrangian and Stokes drift velocities are obtained for plane-wave and Jacobi elliptic function solutions of the nonlinear Schrödinger equation. Numerical approximations to particle trajectories for these solutions are found and the Lagrangian and Stokes drift velocities corresponding to these numerical solutions corroborate the theoretical results. We show that background currents have significant effects on the mean transport properties of waves. In particular, certain combinations of background shear and carrier wave frequency lead to the disappearance of mean-surface mass transport. These results provide a possible explanation for the measurements reported in Smith (J. Phys. Oceanogr., vol. 36, 2006, pp. 1381–1402). Our results also provide further evidence of the viability of the modification of the Stokes drift velocity beyond the standard monochromatic approximation, such as recently proposed in Breivik et al. (J. Phys. Oceanogr., vol. 44, 2014, pp. 2433–2445) in order to obtain a closer match to a range of complex ocean wave spectra.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Figure 1. MIs exist – white, MIs suppressed – black, for $\tilde{\unicode[STIX]{x1D70E}}=10^{-3}$ (a), $\tilde{\unicode[STIX]{x1D70E}}=10^{-5}$ (b), $\tilde{\unicode[STIX]{x1D70E}}=10^{-5}$ (c) and $\tilde{\unicode[STIX]{x1D70E}}=0$ (d). Note the change in scale of the axes in (c) and (d) relative to (a) and (b). Note, while we assumed that $\unicode[STIX]{x1D714}=O(1)$ in our derivation of the NLS equation, to see the impact of surface tension and its connection to MI, we have had to plot on an exaggerated scale in this figure.

Figure 1

Figure 2. Plot of the zero set $u_{p}^{L}(k_{0},\unicode[STIX]{x1D714})=0$. The dot denotes the point $(k_{0},\unicode[STIX]{x1D714})=(1,1.6818)$.

Figure 2

Figure 3. Log plot of the surface SDV parameter $\tilde{u} ^{S}(k_{0},\unicode[STIX]{x1D714})$. The curves along which $\tilde{u} ^{S}(k_{0},\unicode[STIX]{x1D714})=0$ mirror the transitions between MI stable and unstable regions seen in figure 1. The surface SDV is most augmented near the curves corresponding to $\unicode[STIX]{x1D6FC}_{nl}(k_{0},\unicode[STIX]{x1D714})=0$.

Figure 3

Figure 4. Plots of $\tilde{u} ^{S}(1,\unicode[STIX]{x1D714})$ for $-1\leqslant \unicode[STIX]{x1D714}\leqslant 4$ (a), $-1\leqslant \unicode[STIX]{x1D714}\leqslant 1.12$ (b) and $1.17\leqslant \unicode[STIX]{x1D714}\leqslant 4$ (c). Note, $\unicode[STIX]{x1D6FC}_{nl}(1;1.1550)=0$. This shows that the magnitude of the SDV increases with increasing shear on the focusing side of the singularity (b), and decreases with increasing shear on the defocusing side (c).

Figure 4

Figure 5. Strength of the surface velocity as measured via plots of $\sqrt{2|\unicode[STIX]{x1D6FC}_{d}/\unicode[STIX]{x1D6FC}_{nl}|}$ for $k_{0}=1$ for $-1\leqslant \unicode[STIX]{x1D714}\leqslant 4$ (a), $-1\leqslant \unicode[STIX]{x1D714}\leqslant 1.12$ (b) and $1.17\leqslant \unicode[STIX]{x1D714}\leqslant 4$ (c). Increasing shear increases the velocity on the focusing side, and decreases it on the defocusing side.

Figure 5

Figure 6. Focusing case – plots of particle paths correspond to the solution given in (2.38) with $\unicode[STIX]{x1D716}=0.1$, $\unicode[STIX]{x1D6FD}=1$, $k_{0}\approx 1$, $\unicode[STIX]{x1D705}=0.5$, with $\unicode[STIX]{x1D714}=0$ (a), $\unicode[STIX]{x1D714}=1.12$ (b) and $\unicode[STIX]{x1D714}=-1$ (c). The grey dots indicate the starting positions of the tracers while the black dots indicate their final positions.

Figure 6

Figure 7. Focusing case – plots of particle paths correspond to the solution given in (2.38) with $\unicode[STIX]{x1D716}=0.1$, $\unicode[STIX]{x1D6FD}=1$, $k_{0}\approx 1$, $\unicode[STIX]{x1D705}=0.99$, with $\unicode[STIX]{x1D714}=0$ (a), $\unicode[STIX]{x1D714}=1.12$ (b) and $\unicode[STIX]{x1D714}=-1$ (c). The grey dot indicates the starting position of the tracer while the black dot indicates the final position.

Figure 7

Figure 8. Defocusing case – plots of particle paths correspond to the solution given in (2.40) with $\unicode[STIX]{x1D716}=0.1$, $\unicode[STIX]{x1D6FD}=1$, $k_{0}\approx 1$, with $\unicode[STIX]{x1D705}=0.5$ (a), $\unicode[STIX]{x1D705}=0.99$ (b). The choices of $\unicode[STIX]{x1D714}$ ensure that $\tilde{u} ^{L}(1,\unicode[STIX]{x1D714})=0$, see figure 2, thereby leading to the nearly closed, elliptical particle paths. The grey dots indicate the starting positions of the tracers while the black dots indicate their final positions.

Figure 8

Figure 9. Defocusing case – plot of a particle path corresponding to a plane-wave solution with $\unicode[STIX]{x1D716}=0.1$, $A=1$, $k_{0}=1$ and $\unicode[STIX]{x1D714}=1.6818$, which ensures that $\tilde{u} ^{L}(1,\unicode[STIX]{x1D714})=0$, see figure 2, thereby leading to the nearly closed, elliptical particle paths. The grey dots indicate the starting positions of the tracers while the black dots indicate their final positions.

Figure 9

Figure 10. Defocusing – near dark-soliton solution for $k_{0}\approx 1$, $\unicode[STIX]{x1D705}=0.99$ and $\unicode[STIX]{x1D714}=1.17$ (a) and $\unicode[STIX]{x1D714}=4$ (b). The grey dot indicates the starting position of the tracer while the black dot indicates the final position.

Figure 10

Figure 11. Defocusing case – plane-wave solution for $k_{0}=1$, $\unicode[STIX]{x1D714}=4$, $A=1$, with (b) providing a detail of (a). The grey dot indicates the starting position of the tracer while the black dot indicates the final position.