Shao-Ping, Nonlinear acoustic-optical effect and extraordinary diffraction distribution in liquid surface. Vibration and Sound (McGraw-Hill, New York, 1948), p. Morse, Acoustical Society of America, American Institute of Physics. Fort, Single-particle diffraction and interference at a macroscopic scale. Gautier et al., From bouncing to floating: noncoalescence of drops on a fluid bath. Thus, a sound with a wavelength of 34 cm in air (1,000 Hz) will not be hampered by an object that is less than 34 cm in diameter, but a larger object may. Su et al., Visualizing detecting low-frequency underwater acoustic signals by means of optical diffraction. Wang et al., Angle compensation and asymmetry effect of light diffracted by millimeter liquid surface slosh wave. Wang, Small amplitude liquid surface sloshing process detected by optical method. Pingping et al., Low-gravity liquid nonlinear sloshing analysis in a tank under pitching excitation. Empirical acousto-optic sonar performance versus water surface condition, in MTS/IEEE Oceans 2001. Antonelli, Experimental detection and reception performance for uplink underwater acoustic communication using a remote, in-air, acousto-optic sensor. Buhrow, Direct measurement of the attenuation of capillary waves by laser interferometry: noncontact determination of viscosity. Visible light of wavelength 550 nm falls on a single slit and produces its second diffraction minimum at an angle of 45.0 relative to the incident direction of the light, as in Figure 4.2.5 4.2. Separation occurs when the refractive index inside the prism varies with wavelength, so different wavelengths propagate at different speeds inside the prism, causing them to refract at different angles.F. In fact, the central maximum is six times higher than shown here. The variation in speed of light with wavelength is known as dispersion, and is also responsible for the familiar phenomenon in which light is separated into component colors by a prism. In acoustics, where a medium is essential for the waves to exist, the wavelength value is given for a specified medium. When wavelengths of electromagnetic radiation are quoted, the wavelength in vacuum usually is intended unless the wavelength is specifically identified as the wavelength in some other medium. The wavelength λ of a sinusoidal waveform traveling at constant speed v In linear media, any wave pattern can be described in terms of the independent propagation of sinusoidal components. The name originated with the visible light spectrum but now can be applied to the entire electromagnetic spectrum as well as to a sound spectrum or vibration spectrum. The range of wavelengths or frequencies for wave phenomena is called a spectrum. In a crystal lattice vibration, atomic positions vary. Water waves are variations in the height of a body of water. A sound wave is a variation in air pressure, while in light and other electromagnetic radiation the strength of the electric and the magnetic field vary. Examples of waves are sound waves, light, water waves and periodic electrical signals in a conductor. Wavelength depends on the medium (for example, vacuum, air, or water) that a wave travels through. Īssuming a sinusoidal wave moving at a fixed wave speed, wavelength is inversely proportional to the frequency of the wave: waves with higher frequencies have shorter wavelengths, and lower frequencies have longer wavelengths. The term "wavelength" is also sometimes applied to modulated waves, and to the sinusoidal envelopes of modulated waves or waves formed by interference of several sinusoids. Wavelength is commonly designated by the Greek letter lambda (λ). The inverse of the wavelength is called the spatial frequency. Wavelength is a characteristic of both traveling waves and standing waves, as well as other spatial wave patterns. In other words, it is the distance between consecutive corresponding points of the same phase on the wave, such as two adjacent crests, troughs, or zero crossings. In physics and mathematics, wavelength or spatial period of a wave or periodic function is the distance over which the wave's shape repeats. The wavelength of a sine wave, λ, can be measured between any two points with the same phase, such as between crests (on top), or troughs (on bottom), or corresponding zero crossings as shown. For other uses, see Wavelength (disambiguation).
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