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  2. Crest and trough - Wikipedia

    en.wikipedia.org/wiki/Crest_and_trough

    A crest is a point on a surface wave where the displacement of the medium is at a maximum. A trough is the opposite of a crest, so the minimum or lowest point of the wave. When the crests and troughs of two sine waves of equal amplitude and frequency intersect or collide, while being in phase with each other, the result is called constructive ...

  3. Breaking wave - Wikipedia

    en.wikipedia.org/wiki/Breaking_wave

    The outcome is the rapid movement of the base of the wave up the swash slope and the disappearance of the wave crest. The front face and crest of the wave remain relatively smooth with little foam or bubbles, resulting in a very narrow surf zone, or no breaking waves at all. The short, sharp burst of wave energy means that the swash/backwash ...

  4. Rogue wave - Wikipedia

    en.wikipedia.org/wiki/Rogue_wave

    Images from the 2019 simulation of the Draupner wave show how the steepness of the wave forms, and how the crest of a rogue wave breaks when waves cross at different angles. (Click image for full resolution) In the first row (0°), the crest breaks horizontally and plunges, limiting the wave size.

  5. Wave height - Wikipedia

    en.wikipedia.org/wiki/Wave_height

    Wave characteristics. In fluid dynamics, the wave height of a surface wave is the difference between the elevations of a crest and a neighboring trough. [1] Wave height is a term used by mariners, as well as in coastal, ocean and naval engineering.

  6. Wave nonlinearity - Wikipedia

    en.wikipedia.org/wiki/Wave_nonlinearity

    Wave asymmetry indicates the leaning forward or backward of the wave, with a steep front face and a gentle rear face. A steep front correlates with an upward tilt, a steep back is correlated with a downward tilt. The duration and height of the wave-crest equal the duration and height of the wave-trough.

  7. Airy wave theory - Wikipedia

    en.wikipedia.org/wiki/Airy_wave_theory

    Particle motion in an ocean wave at deep (A) and shallow (B) depths. 1) Propagation direction. 2) Wave crest. 3) Wave trough. Underneath the surface, there is a fluid motion associated with the free surface motion. While the surface elevation shows a propagating wave, the fluid particles are in an orbital motion.

  8. Why We Can’t Look Away From Scammer Stories - AOL

    www.aol.com/why-t-look-away-scammer-201349110.html

    A new wave of female-scammer content confirms that Grifter Season was more than just a passing trend. ... comes at the crest of the latest wave of scam content.

  9. Wave interference - Wikipedia

    en.wikipedia.org/wiki/Wave_interference

    If a crest of a wave meets a crest of another wave of the same frequency at the same point, then the amplitude is the sum of the individual amplitudes—this is constructive interference. If a crest of one wave meets a trough of another wave, then the amplitude is equal to the difference in the individual amplitudes—this is known as ...