Journal articles: 'Surface waves'

1

Daigle, G. A. "Surface waves above porous ground surfaces." Journal of the Acoustical Society of America 85, S1 (May 1989): S82. http://dx.doi.org/10.1121/1.2027167.

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2

Torner, Lluis, David Artigas, and Osamu Takayama. "Dyakonov Surface Waves." Optics and Photonics News 20, no. 12 (December 1, 2009): 25. http://dx.doi.org/10.1364/opn.20.12.000025.

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3

Cronin-Golomb, Mark. "Photorefractive surface waves." Optics Letters 20, no. 20 (October 15, 1995): 2075. http://dx.doi.org/10.1364/ol.20.002075.

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4

King, R. "Electromagnetic surface waves." IEEE Antennas and Propagation Society Newsletter 28, no. 6 (1986): 4–11. http://dx.doi.org/10.1109/map.1986.27883.

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5

Camley, R. E. "Nonreciprocal surface waves." Surface Science Reports 7, no. 3-4 (July 1987): 103–87. http://dx.doi.org/10.1016/0167-5729(87)90006-9.

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6

Hess, P. "Surface Acoustic Waves." Applied Physics A Materials Science & Processing 61, no. 3 (September 1995): 227. http://dx.doi.org/10.1007/bf01538186.

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7

HWUNG, HWUNG-HWENG, RAY-YENG YANG, and IGOR V. SHUGAN. "Exposure of internal waves on the sea surface." Journal of Fluid Mechanics 626 (May 10, 2009): 1–20. http://dx.doi.org/10.1017/s0022112008004758.

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We theoretically analyse the impact of subsurface currents induced by internal waves on nonlinear Stokes surface waves. We present analytical and numerical solutions of the modulation equations under conditions that are close to group velocity resonance. Our results show that smoothing of the downcurrent surface waves is accompanied by a relatively high-frequency modulation, while the profile of the opposing current is reproduced by the surface wave's envelope. We confirm the possibility of generating an internal wave forerunner that is a modulated surface wave packet. Long surface waves can create such a wave modulation forerunner ahead of the internal wave, while other relatively short surface waves comprise the trace of the internal wave itself. Modulation of surface waves by a periodic internal wavetrain may exhibit a characteristic period that is less than the internal wave period. This period can be non-uniform while the wave crosses the current zone. Our results confirm that surface wave excitation by means of internal waves, as observed at their group resonance frequencies, is efficient only in the context of opposing currents.

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8

ZHANG, X. "Short surface waves on surface shear." Journal of Fluid Mechanics 541, no. -1 (October 11, 2005): 345. http://dx.doi.org/10.1017/s0022112005006063.

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9

Büscher, H., W. Klein-Heßling, and W. Ludwig. "Surface phonons and elastic surface waves." Annalen der Physik 505, no. 2 (1993): 159–79. http://dx.doi.org/10.1002/andp.19935050208.

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10

Baev, A. R., A. L. Mayorov, M. V. Asadchaya, G. E. Konovalov, and O. S. Sergeeva. "TRANSFORMATION AND SCATTERING OF SURFACE WAVES ON THE ACOUSTIC LOAD TO ULTRASONIC EVALUATION AND MEASUREMENTS. Part 2. The object to study – solid with ledge." Devices and Methods of Measurements 9, no. 2 (June 15, 2018): 142–54. http://dx.doi.org/10.21122/2220-9506-2018-9-2-142-154.

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The lack of information about the features of processes of the surface wave's transformation into volume waves and its scattering in metal objects with ledge, slots, grooves and the others is one of the obstacles to improve of the acoustical testing reliability and widening of technical application. The aim of this work was to study of mechanism of acoustical mode's transformation and determination the laws of the fields forming of scatted volume edge wave's in solids with ledge of different geometry and to suggest direction of the study application in area of acoustical testing and measurements.The features of transformation of surface waves into edge transverse and longitudinal wave modes scatted and their fields forming in the volume of the object with ledge vs. its angle of the slope front surface side (0–135°) and a dimensionless transition radius (0–10,2) varied were studied. Theoretical analysis and experimental data shown that in general case the field of the edge transverse waves in the volume of ledge can be imagined as a superposition of the field of edge waves (scatted on ledge) and accompany waves too, radiated simultaneously with the surface waves to radiate. If dimensionless size of the ledge's transition radius lesser than 1 the resulting field of the edge transverse waves is the summary field of two sources. One of them (with small aperture) is localized in the vicinity of the place of intersection of contact surface with ledge's front side surface. As it was found, the second source of the edge transverse waves – the edge head longitudinal waves to appear in the results of transformation of surface waves on the ledge′s radius transition. The structure of the edge acoustic fields including their extremes vs. ledge's angle and its radius transition, position of the surface wave's probe were experimentally studied and theoretically analyzed.Some directions of the results of researches using are the next: а) ultrasonic testing of hard-to-make technological objects in which defects have low sound reflection; b) ultrasonic structure diagnostics of solid (specimens) set far from the ultrasonic by using edge volume transverse and longitudinal modes; c) creation of new ultrasonic arrangements to sound and to receive transverse waves of different polarization.

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11

Wang, Letian, Min Zhang, and Jiong Liu. "Electromagnetic Scattering Model for Far Wakes of Ship with Wind Waves on Sea Surface." Remote Sensing 13, no. 21 (November 3, 2021): 4417. http://dx.doi.org/10.3390/rs13214417.

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A comprehensive electromagnetic scattering model for ship wakes on the sea surface is proposed to study the synthetic aperture radar (SAR) imagery for ship wakes. Our model considers a coupling of various wave systems, including Kelvin wake, turbulent wake, and the ocean ambient waves induced by the local wind. The fluid–structure coupling between the ship and the water surface is considered using the Reynolds–averaged Navier–Stokes (RANS) equation, and the wave–current effect between the ship wake and wind waves is considered using the wave modulation model. The scattering model can better describe the interaction of the ship wakes on sea surface and illustrates well the features of the ship wakes with local wind waves in SAR images.

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12

Mackay, Tom G., Chenzhang Zhou, and Akhlesh Lakhtakia. "Dyakonov–Voigt surface waves." Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 475, no. 2228 (August 2019): 20190317. http://dx.doi.org/10.1098/rspa.2019.0317.

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Electromagnetic surface waves guided by the planar interface of an isotropic dielectric medium and a uniaxial dielectric medium, both non-dissipative, were considered, the optic axis of the uniaxial medium lying in the interface plane. Whereas this interface is known to support the propagation of Dyakonov surface waves when certain constraints are satisfied by the constitutive parameters of the two partnering mediums, we identified a different set of constraints that allow the propagation of surface waves of a new type. The fields of the new surface waves, named Dyakonov–Voigt (DV) surface waves, decay as the product of a linear and an exponential function of the distance from the interface in the anisotropic medium, whereas the fields of the Dyakonov surface waves decay only exponentially in the anisotropic medium. In contrast to Dyakonov surface waves, the wavenumber of a DV surface wave can be found analytically. Also, unlike Dyakonov surface waves, DV surface waves propagate only in one direction in each quadrant of the interface plane.

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13

Paknys, R., and D. R. Jackson. "The relation between creeping waves, leaky waves, and surface waves." IEEE Transactions on Antennas and Propagation 53, no. 3 (March 2005): 898–907. http://dx.doi.org/10.1109/tap.2004.842625.

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14

Sun, Zhijun, Xiaoliu Zuo, Tengpeng Guan, and Wei Chen. "Artificial TE-mode surface waves at metal surfaces mimicking surface plasmons." Optics Express 22, no. 4 (February 21, 2014): 4714. http://dx.doi.org/10.1364/oe.22.004714.

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15

Kenyon, Kern E. "Frictionless Surface Gravity Waves." Natural Science 12, no. 04 (2020): 199–201. http://dx.doi.org/10.4236/ns.2020.124017.

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16

Ignatovich, V. K. "On neutron surface waves." Crystallography Reports 54, no. 1 (January 2009): 116–21. http://dx.doi.org/10.1134/s1063774509010209.

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17

Snouck, Daniel, Mark-Tiele Westra, and Willem van de Water. "Turbulent parametric surface waves." Physics of Fluids 21, no. 2 (February 2009): 025102. http://dx.doi.org/10.1063/1.3075951.

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18

Malischewsky, Peter, and M. A. Breazeale. "Surface Waves and Discontinuities." Journal of the Acoustical Society of America 88, no. 1 (July 1990): 588. http://dx.doi.org/10.1121/1.399904.

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19

Datsko, V. N., and A. A. Kopylov. "On surface electromagnetic waves." Physics-Uspekhi 51, no. 1 (January 31, 2008): 101–2. http://dx.doi.org/10.1070/pu2008v051n01abeh006208.

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20

Datsko, V. N., and A. A. Kopylov. "On surface electromagnetic waves." Uspekhi Fizicheskih Nauk 178, no. 1 (2008): 109. http://dx.doi.org/10.3367/ufnr.0178.200801f.0109.

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21

Garanovich, Ivan L., Alexander Szameit, Andrey A. Sukhorukov, Stefan Nolte, Thomas Pertsch, Andreas Tünnermann, and Yuri S. Kivshar. "Defect-Free Surface Waves." Optics and Photonics News 19, no. 12 (December 1, 2008): 26. http://dx.doi.org/10.1364/opn.19.12.000026.

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22

Neducza, Boriszláv. "Stacking of surface waves." GEOPHYSICS 72, no. 2 (March 2007): V51—V58. http://dx.doi.org/10.1190/1.2431635.

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The seismic surface wave method (SWM) is a powerful means of characterizing near-surface structures. Although the SWM consists of only three steps (data acquisition, determination of dispersion curves, and inversion), it is important to take considerable care with the second step, determination of the dispersion curves. This step is usually completed by spectral analysis of surface waves (SASW) or multichannel analysis of surface waves (MASW). However, neither method is ideal, as each has its advantages and disadvantages. SASW provides higher horizontal resolution, but it is very sensitive to coherent noise and individual geophone coupling. MASW is a robust method able to separate different wave types, but its horizontal resolution is lower. Stacking of surface waves (SSW) is a good compromise between SASW and MASW. Using a reduced number of traces increases the horizontal resolution of MASW, and utilizing other shot records with the same receivers compensates for the decreased signal-to-noise ratio. The stacking is realized by summing the [Formula: see text] amplitude spectra of windowed shot records, where windowing produces higher horizontal resolution and stacking produces improved data quality. Mixing is applied between the stacks derived with different parameters, as different frequency ranges require different windowing. SSW was tested and corroborated on a deep seismic data set. Horizontal resolution is validated by [Formula: see text] plots at different frequencies, and [Formula: see text] plots present data quality.

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23

Tizianel, Julian, Jean F. Allard, and Bruno Brouard. "Surface waves above honeycombs." Journal of the Acoustical Society of America 104, no. 4 (October 1998): 2525–28. http://dx.doi.org/10.1121/1.423908.

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24

Schewe, Phillip F. "Surface acoustic waves (SAWs)." Physics Today 59, no. 6 (June 2006): 21. http://dx.doi.org/10.1063/1.4797385.

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25

Lundquist, Paul B., and David R. Andersen. "Uniaxial nonlinear surface waves." Physical Review E 53, no. 4 (April 1, 1996): 4077–83. http://dx.doi.org/10.1103/physreve.53.4077.

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26

Lundquist, Paul B., David R. Andersen, and Pascal Morel. "Biaxial nonlinear surface waves." Physical Review E 54, no. 4 (October 1, 1996): 4375–83. http://dx.doi.org/10.1103/physreve.54.4375.

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27

Galiev, Sh U., and T. Sh Galiev. "Resonant travelling surface waves." Physics Letters A 246, no. 3-4 (September 1998): 299–305. http://dx.doi.org/10.1016/s0375-9601(98)00414-9.

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28

Moslem, W. M., P. K. Shukla, and B. Eliasson. "Surface plasma rogue waves." EPL (Europhysics Letters) 96, no. 2 (September 27, 2011): 25002. http://dx.doi.org/10.1209/0295-5075/96/25002.

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29

Ren, X. K., D. Y. Yang, T. H. Zhang, S. Zhang, L. Zhou, J. G. Tian, and J. J. Xu. "Polymeric photorefractive surface waves." Optics Communications 283, no. 19 (October 2010): 3792–97. http://dx.doi.org/10.1016/j.optcom.2010.05.032.

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30

Pizzo, Nick E. "Surfing surface gravity waves." Journal of Fluid Mechanics 823 (June 16, 2017): 316–28. http://dx.doi.org/10.1017/jfm.2017.314.

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A simple criterion for water particles to surf an underlying surface gravity wave is presented. It is found that particles travelling near the phase speed of the wave, in a geometrically confined region on the forward face of the crest, increase in speed. The criterion is derived using the equation of John (Commun. Pure Appl. Maths, vol. 6, 1953, pp. 497–503) for the motion of a zero-stress free surface under the action of gravity. As an example, a breaking water wave is theoretically and numerically examined. Implications for upper-ocean processes, for both shallow- and deep-water waves, are discussed.

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31

Cramer, N. F. "Nonlinear surface Alfvén waves." Journal of Plasma Physics 46, no. 1 (August 1991): 15–27. http://dx.doi.org/10.1017/s0022377800015920.

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The problem of nonlinear surface Alfvén waves propagating on an interface between a plasma and a vacuum is discussed, with dispersion provided by the finite-frequency effect, i.e. the finite ratio of the frequency to the ion-cyclotron frequency. A set of simplified nonlinear wave equations is derived using the method of stretched co-ordinates, and another approach uses the generation of a second-harmonic wave and its interaction with the first harmonic to obtain a nonlinear dispersion relation. A nonlinear Schrödinger equation is then derived, and soliton solutions found that propagate as solitary pulses in directions close to parallel and antiparallel to the background magnetic field.

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32

Nalimov, V. I. "Nonstationary vortex surface waves." Siberian Mathematical Journal 37, no. 6 (November 1996): 1189–98. http://dx.doi.org/10.1007/bf02106744.

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33

Hudson, J. A. "Surface waves and discontinuities." Physics of the Earth and Planetary Interiors 54, no. 3-4 (April 1989): 388–89. http://dx.doi.org/10.1016/0031-9201(89)90259-8.

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34

Nolet, Guust. "Surface waves and discontinuities." Tectonophysics 172, no. 3-4 (February 1990): 371–72. http://dx.doi.org/10.1016/0040-1951(90)90045-a.

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35

Miles, J., and D. Henderson. "Parametrically Forced Surface Waves." Annual Review of Fluid Mechanics 22, no. 1 (January 1990): 143–65. http://dx.doi.org/10.1146/annurev.fl.22.010190.001043.

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36

Armstrong, Seiji. "Diffraction-free surface waves." Nature Photonics 6, no. 11 (November 2012): 720. http://dx.doi.org/10.1038/nphoton.2012.271.

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37

Miles, Alan J., and B. Roberts. "Magnetoacoustic-gravity surface waves." Solar Physics 141, no. 2 (October 1992): 205–34. http://dx.doi.org/10.1007/bf00155176.

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38

Miles, Alan J., H. R. Allen, and B. Roberts. "Magnetoacoustic-gravity surface waves." Solar Physics 141, no. 2 (October 1992): 235–51. http://dx.doi.org/10.1007/bf00155177.

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39

Austria, Lawrence, and John K. Hunter. "Nonlinear variational surface waves." Communications in Information and Systems 13, no. 1 (2013): 3–43. http://dx.doi.org/10.4310/cis.2013.v13.n1.a1.

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40

Stenflo, L., and M. Y. Yu. "Nonlinear spherical surface waves." Physical Review A 42, no. 8 (October 1, 1990): 4894–97. http://dx.doi.org/10.1103/physreva.42.4894.

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41

TRAN, H. T. "QUADRATIC NONLINEAR SURFACE WAVES." Journal of Nonlinear Optical Physics & Materials 05, no. 01 (January 1996): 133–38. http://dx.doi.org/10.1142/s021886359600012x.

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Nonlinear surface waves at an interface between a linear medium and another medium with quadratic nonlinearity are possible due to the phenomenon of nonlinearity-induced phase matching. The waves are numerically calculated, along with their dispersion, stability, and comparison with their cubic counterparts. An extension to guided waves is also discussed.

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42

Salvo, E. Di. "Orbiting and surface waves." Journal of Physics A: Mathematical and General 19, no. 2 (February 1, 1986): L37—L40. http://dx.doi.org/10.1088/0305-4470/19/2/003.

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43

Parker, D. F., and E. A. David. "Nonlinear piezoelectric surface waves." International Journal of Engineering Science 27, no. 5 (January 1989): 565–81. http://dx.doi.org/10.1016/0020-7225(89)90008-6.

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44

Akhmediev, N. N., R. F. Nabiev, and Yu M. Popov. "Stripe nonlinear surface waves." Solid State Communications 66, no. 9 (June 1988): 981–85. http://dx.doi.org/10.1016/0038-1098(88)90550-9.

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45

Gonz�lez, Alejandro G., and Julio Gratton. "Magnetoacoustic surface gravity waves." Solar Physics 134, no. 2 (August 1991): 211–32. http://dx.doi.org/10.1007/bf00152645.

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46

Suzuki, Nobuhiro, Baylor Fox‐Kemper, Peter E. Hamlington, and Luke P. Van Roekel. "Surface waves affect frontogenesis." Journal of Geophysical Research: Oceans 121, no. 5 (May 2016): 3597–624. http://dx.doi.org/10.1002/2015jc011563.

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47

McWilliams, James C. "Surface wave effects on submesoscale fronts and filaments." Journal of Fluid Mechanics 843 (March 22, 2018): 479–517. http://dx.doi.org/10.1017/jfm.2018.158.

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A diagnostic analysis is made for the ageostrophic secondary circulation, buoyancy flux and frontogenetic tendency (SCFT) in upper-ocean submesoscale fronts and dense filaments under the combined influences of boundary-layer turbulent mixing, surface wind stress and surface gravity waves. The analysis is based on a momentum-balance approximation that neglects ageostrophic acceleration, and the surface wave effects are represented with a wave-averaged asymptotic theory based on the time scale separation between wave and current evolution. The wave’s Stokes-drift velocity $\boldsymbol{u}_{st}$ induces SCFT effects that are dominant in strong swell with weak turbulent mixing, and they combine with Ekman and turbulent thermal wind influences in more general situations near wind–wave equilibrium. The complementary effect of the submesoscale currents on the waves is weak for longer waves near the wind–wave or swell spectrum peak, but it is strong for shorter waves.

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48

Zhou, Chenzhang, Tom G. Mackay, and Akhlesh Lakhtakia. "Theory of Dyakonov–Tamm surface waves featuring Dyakonov–Tamm–Voigt surface waves." Optik 211 (June 2020): 164575. http://dx.doi.org/10.1016/j.ijleo.2020.164575.

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49

Rutgersson, Anna, Øyvind Sætra, Alvaro Semedo, Björn Carlsson, and Rajesh Kumar. "Impact of surface waves in a Regional Climate Model." Meteorologische Zeitschrift 19, no. 3 (June 1, 2010): 247–57. http://dx.doi.org/10.1127/0941-2948/2010/0456.

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50

Skalsky, V. R., and O. M. Mokryy. "Michelson interferometer stabilized scheme for surface acoustic waves detecting." Information extraction and processing 2019, no. 47 (December 26, 2019): 40–46. http://dx.doi.org/10.15407/vidbir2019.47.040.

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Journal articles on the topic 'Surface waves'

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