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Surface waves span a wide frequency range, and the period of waves that are most damaging is usually 10 seconds or longer. Surface waves can travel around the globe many times from the largest earthquakes. Surface waves are caused when P waves and S waves come to the surface. Examples are the waves at the surface of water and air (ocean surface ...
A Scholte wave is a surface wave (interface wave) propagating at an interface between a fluid and an elastic solid medium (such as an interface between water and sand). [1] [2] The wave is of maximum intensity at the interface and decreases exponentially away from the interface into both the fluid and the solid medium. [3]
Ground waves propagate parallel to and adjacent to the surface of the Earth, and are capable of covering long distances by diffracting around the Earth's curvature. This radiation is also known as the Norton surface wave , or more properly the Norton ground wave , because ground waves in radio propagation are not confined to the surface.
Rayleigh waves are generated by the interaction of P- and S- waves at the surface of the earth, and travel with a velocity that is lower than the P-, S-, and Love wave velocities. Rayleigh waves emanating outward from the epicenter of an earthquake travel along the surface of the earth at about 10 times the speed of sound in air (0.340 km/s ...
Animation of an electron transported via a surface acoustic wave. Even at the smallest scales of current semiconductor technology, each operation is carried out by huge streams of electrons. [22] Reducing the number of electrons involved in these processes, with the ultimate goal of achieving single electron control is a serious challenge.
Edge wave, a surface gravity wave fixed by refraction against a rigid boundary; Faraday wave, a type of wave in liquids; Gravity wave, in fluid dynamics; Internal wave, a wave within a fluid medium; Shock wave, in aerodynamics; Sound wave, a wave of sound through a medium such as air or water; Tidal wave, a scientifically incorrect name for a ...
Stokes drift – Average velocity of a fluid parcel in a gravity wave; Undertow (water waves) – Return flow below nearshore water waves. Ursell number – Dimensionless number indicating the nonlinearity of long surface gravity waves on a fluid layer. Wave shoaling – Effect by which surface waves entering shallower water change in wave height
How Love waves work. In elastodynamics, Love waves, named after Augustus Edward Hough Love, are horizontally polarized surface waves.The Love wave is a result of the interference of many shear waves guided by an elastic layer, which is welded to an elastic half space on one side while bordering a vacuum on the other side.