Crest and Trough
Crest and trough are fundamental concepts in the study of waves, particularly transverse waves, which displace their medium perpendicular to the energy transfer direction. The crest represents the maximum height of the wave, which is the point of greatest positive displacement from the rest position, while the trough indicates the minimum depth, marking the greatest negative displacement. The distance between two consecutive crests or troughs defines the wavelength, and the amplitude, or the wave's height, is half the distance between the crest and trough.
Wave interactions are influenced by their phase relationships—waves in sync enhance each other through constructive interference, while waves in antiphase diminish one another through destructive interference. Understanding these properties is essential in various fields, such as physics, engineering, and oceanography, as they convey important information about the wave's energy transmission capabilities and behaviors. High-energy waves typically exhibit short wavelengths and high frequencies, whereas low-energy waves have longer wavelengths and lower frequencies. Observing crests and troughs can provide insight into wave dynamics and their potential interactions in different media.
Crest and Trough
FIELDS OF STUDY: Classical Mechanics; Fluid Mechanics; Electromagnetism
ABSTRACT: In a transverse wave (e.g. an ocean wave), the crest is the highest point of the wave and the trough is the lowest point. Measurements based on crests and troughs reveal a wave’s wavelength and amplitude. When two waves interact, the relative positions of crests and troughs determines whether they will boost one another or cancel each other out.
PRINCIPAL TERMS
- amplitude: the maximum amount of displacement at a point on the wave from its position of rest.
- antiphase: waves with a phase difference of 180 degrees relative to one another. The crests of one wave align with the troughs of the other and vice versa.
- constructive interference: when waves meet in the same medium and are in similar phase.
- destructive interference: when waves meet in the same medium and are in dissimilar phase.
- maximum: the point of greatest wave height, also known as a crest or peak. It is the point of greatest positive displacement from the position of rest in a wave.
- minimum: the point of greatest wave depth, also known as a trough or valley. It is the point of greatest negative displacement from the position of rest in a wave.
- transverse: type of wave that displaces its medium perpendicular to the direction of energy transfer. Ocean waves, for example, move water vertically but transmit energy horizontally across the surface.
- wavelength: the full length of a complete wave cycle, measured as the distance between crests of a wave.
- revolution: describes circular motion wherein an object circles an internal axis (e.g. the moon spinning about its axis); contrast to rotation, wherein the axis is external (e.g. the moon orbiting the earth).
Crests, Troughs, and Wave Properties
In a transverse wave—which displaces its medium perpendicular to the transfer of energy—the crests and troughs are the areas of maximum and minimum height from the resting position (equilibrium), respectively. The distance between two crests or two troughs is the wavelength of a wave. The distance between the top of a crest or bottom of a trough relative to the equilibrium position—such as the flat surface of the sea in an ocean wave—determines the wave’s amplitude. A concept related to wavelength is frequency, or the number of waves per unit of time.
These properties reveal important information about the energy transmission ability of a wave. A long wavelength indicates a lower capacity for energy transfer over time. A large amplitude indicates a high energy content in each cycle of the wave. High-energy waves have short wavelengths and high frequencies. Low-energy waves have long wavelengths and low frequencies.
Interference and Phase
The orientation of crests and troughs is determined by a wave’s phase. Two waves of the same frequency are said to be in antiphase relative to one another if the crests of one wave line up with the troughs of the other. When two waves traveling through the same medium encounter one another, their relative phase determines the nature of their interaction. If they are in sync, with crests corresponding to crests, the waves will reinforce one another. This is constructive interference. If they are in antiphase, they will dampen each other. This is destructive interference. Careful observation of crests and troughs can reveal crucial information about transverse waves and their potential interactions.

Bibliography
"Anatomy of an Electromagnetic Wave." Mission: Science. NASA, n.d. Web. 19 June 2015.
Fleisch, Daniel, and Laura Kinnaman. A Student’s Guide to Waves. New York: Cambridge UP, 2015. Print.
Freegarde, Tim. Introduction to the Physics of Waves. Cambridge: Cambridge UP, 2013. Print.
Newton, Roger G. Waves and Particles: Two Essays on Fundamental Physics. Hackensack: World Scientific, 2014. Print.
Pain, H. J., and Patricia Rankin. Introduction to Vibrations and Waves. Hoboken: Wiley, 2015. Print.
Russell, Daniel A. "Longitudinal and Transverse Wave Motion." Acoustics and Vibration Animations. Pennsylvania State U, 18 Feb. 2015. Web. 19 June 2015.