The proper name for the height of a wave is its amplitude. It refers to the distance from the midpoint (resting position) of the wave to the peak (crest) or trough (lowest point).
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The amplitude of a wave is a measure of its maximum displacement from the equilibrium position. As the height of a wave increases, the maximum displacement of the particles creating the wave also increases, resulting in a larger amplitude. Therefore, the height of a wave directly affects its amplitude.
The term for the height of a wave is called the amplitude. It is the distance from the equilibrium point of the wave to the peak or trough.
The height of a wave is measured from the centerline, or still water level, to the wave's peak or crest. This measurement is known as the wave height.
The height of a wave is the vertical distance between the wave's crest and trough. It is typically measured in meters, from peak to trough. The height of a wave can vary depending on factors such as wind speed, duration, and fetch.
The height of a wave's trough is typically half the amplitude of the wave. The amplitude is the distance from the equilibrium point (the middle of the wave) to the peak or trough. Thus, the amplitude does have an impact on the height of the wave's trough.