Abstract
The ability to send a wave to fetch an object from a distance would find a broad range of applications. Quasi-standing Faraday waves on water create horizontal vortices1,2, yet it is not known whether propagating waves can generate large-scale flows—small-amplitude irrotational waves only push particles in the direction of propagation3,4,5. Here we show that when waves become three-dimensional as a result of the modulation instability, a floater can be forced to move towards the wave source. The mechanism for this is the generation of surface vortices by waves propagating away from vertically oscillating plungers. We introduce a new conceptual framework for understanding wave-driven flows, which enables us to engineer inward and outward surface jets, stationary vortices, and other complex flows. The results form a new basis for the remote manipulation of objects on fluid surfaces and for a better understanding of the motion of floaters in the ocean, the generation of wave-driven jets, and the formation of Lagrangian coherent structures.
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Acknowledgements
This work was supported by the Australian Research Council’s Discovery Projects funding scheme (DP110101525). H.X. would like to acknowledge the support of the Australian Research Council’s Discovery Early Career Research Award (DE120100364). The authors thank K. Szewc for developing the code for the finite-time Lyapunov exponent analysis used to generate Fig. 4f, and M. Gwynneth for his help with experimental set-up. N.F. acknowledges the help of S. Ramsden of the National Computational Infrastructure, Vizlab, ANU with visualization of 3D flows and trajectories using the Houdini animation software. The research of G.F. was supported by the Minerva Foundation and the Binational Science Foundation (BSF).
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H.P., N.F. and M.S. designed and performed the experiments; H.X., N.F., G.F. and H.P. analysed the data. M.S. and G.F. wrote the paper. All authors discussed and edited the manuscript.
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Punzmann, H., Francois, N., Xia, H. et al. Generation and reversal of surface flows by propagating waves. Nature Phys 10, 658–663 (2014). https://doi.org/10.1038/nphys3041
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DOI: https://doi.org/10.1038/nphys3041
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