Why is the speed of water waves dependent on depth?

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SUMMARY

The speed of water waves is directly influenced by water depth, as described by the equation c = √(gL tanh(2πd/L)). In deep water, where d > L/2, the wave speed simplifies to c = √(gL/2π), while in shallow water, where d << L/2, it becomes c = √(gd). This phenomenon occurs because water particles in deep water move in circular orbits, while shoaling causes these orbits to flatten due to bottom friction, resulting in slower wave speeds in shallower depths. The relationship between wave speed and depth is crucial for understanding wave dynamics in various aquatic environments.

PREREQUISITES
  • Understanding of wave mechanics
  • Familiarity with the concepts of wavelength and water depth
  • Knowledge of hyperbolic functions, specifically tanh
  • Basic principles of fluid dynamics
NEXT STEPS
  • Study the derivation of wave speed equations in fluid dynamics
  • Explore the implications of wave speed on coastal erosion and sediment transport
  • Learn about the effects of wave shoaling on marine navigation
  • Investigate the role of wave speed in tsunami propagation
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Marine scientists, oceanographers, civil engineers, and anyone involved in coastal management or studying wave dynamics will benefit from this discussion.

quantum123
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Why is the speed of water waves dependent on the depth?
 
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The velocity, c, of a simple sinusoidal surface water wave is described by, where L is the wavelength and d the water depth:

c = \sqrt {\frac{{gL\tanh \left( {\frac{{2\pi d}}{L}} \right)}}{{2\pi }}}

Note that when d > L /2

\tanh \left( {\frac{{2\pi d}}{L}} \right) \approx 1

so the velocity for deep water reduces to

c = \sqrt {\frac{{gL}}{{2\pi }}}

and when d << L/2

\tanh \left( {\frac{{2\pi d}}{L}} \right) \approx \left( {\frac{{2\pi d}}{L}} \right)

So the velocity becomes

c = \sqrt {gd}

This is because the water particles are moving in (nearly) circular orbits in deep water. As the water shoals the bottom exerts a drag which elongates the orbit to an ellipse, which gets flatter and flatter with shoaling.
 
Roughly speaking, friction with the bottom slows the wave so that waves in deeper water are faster. The more precise derivation, showing that the wave speed is proportional to the square root of the depth is what studiot gives.
 

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