Difference between revisions of "Refraction"

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[[File:WaveRefraction.jpg|thumb|300px|center|Refraction of obliquely incident waves when entering shallow coastal. Bending of the wave crests to become parallel to the shore. Image Google Earth.]]
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[[File:WaveRefraction.jpg|thumb|300px|right|Refraction of obliquely incident waves when entering shallow coastal. Bending of the wave crests to become parallel to the shore. Image Google Earth.]]
  
  
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==Notes==
  
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When incident waves are approaching the coast from different directions (directional spread), refraction in shallow water will bend the wave fronts such that they become aligned with the depth contours. The directional spread will thus become narrower. 
  
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Wave refraction at any location <math>(x,y)</math> is described by Snell's law
  
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<math>\Large\frac{\sin \theta}{c}\normalsize = constant .</math>
  
==See also==
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Here is <math>\theta</math> the direction of a wave ray and <math>c</math> the wave propagation speed.
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Refraction and [[diffraction]] have to be considered together<ref>Huntley, D.A. and Bryan, K.R. 2022. Waves. Chapter 8.03, Treatise on Geomorphology 2nd edition. Elsevier</ref>, See also Komar 1998<ref>Komar, P.D. 1998. Beach Processes and Sedimentation. Prentice-Hall</ref>.
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==Related articles==
 
:[[Wave transformation]]
 
:[[Wave transformation]]
 
:[[Shallow-water wave theory]]
 
:[[Shallow-water wave theory]]
 
:[[Diffraction]]
 
:[[Diffraction]]
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==References==
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<references/>

Revision as of 13:22, 30 October 2022

Definition of Refraction:
The propensity of waves to align the wave front in shallow water with the depth contour, according to Snell's law. Also: Change of wave propagation direction due to the interaction with currents.
This is the common definition for Refraction, other definitions can be discussed in the article


Refraction of obliquely incident waves when entering shallow coastal. Bending of the wave crests to become parallel to the shore. Image Google Earth.


Notes

When incident waves are approaching the coast from different directions (directional spread), refraction in shallow water will bend the wave fronts such that they become aligned with the depth contours. The directional spread will thus become narrower.

Wave refraction at any location [math](x,y)[/math] is described by Snell's law

[math]\Large\frac{\sin \theta}{c}\normalsize = constant .[/math]

Here is [math]\theta[/math] the direction of a wave ray and [math]c[/math] the wave propagation speed.

Refraction and diffraction have to be considered together[1], See also Komar 1998[2].



Related articles

Wave transformation
Shallow-water wave theory
Diffraction

References

  1. Huntley, D.A. and Bryan, K.R. 2022. Waves. Chapter 8.03, Treatise on Geomorphology 2nd edition. Elsevier
  2. Komar, P.D. 1998. Beach Processes and Sedimentation. Prentice-Hall