Refraction of Waves

5.4 Refraction of Waves
PHYSICS • Form 4 • Chapter 5: Waves

5.4 Refraction of Waves

Refraction of waves is the change in the direction of propagation of waves caused by the change in the velocity of waves when propagating from one medium to another. In water waves, variations in water depth alter wave speed and wavelength, while the frequency remains unchanged. This concept explains natural occurrences such as sea waves curving to follow shorelines and sound being heard more clearly at night than during the day.

Learning Objectives

  • Define the refraction of waves.
  • Describe the effects of refraction on wave characteristics as waves travel between regions of different depths or media.
  • Draw and complete diagrams of refraction of plane water waves approaching a boundary at an angle.
  • Explain daily life and natural phenomena involving wave refraction.
  • Solve numerical problems involving wave refraction using \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\).

Refraction of Water Waves Across Depth Boundaries and Shorelines

See how wave direction, speed and wavelength change between deep and shallow regions, and how this relates to wave behaviour at capes and bays.

Deep to Shallow Water

Deep region Longer wavelength
Shallow region Shorter wavelength

Refraction at a Boundary

Deep waterShallow waterNormalIncident rayRefracted rayir

Short Explanation

What is Refraction of Waves?

Refraction of waves is the change in direction of propagation of waves caused by the change in the velocity of waves when the waves propagate from one medium to another.

Speed Dependencies

Speed of water waves is influenced by the depth of water. Speed of sound waves is influenced by the density of air. Speed of light waves is influenced by the optical density of the medium.

Key Relationship

Since frequency \(f\) remains constant during refraction: \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\) or \(\frac{v_1}{v_2} = \frac{\lambda_1}{\lambda_2}\).

Wave Speed Formula

Wave speed is given by \(v = f\lambda\), so \(f = \frac{v}{\lambda}\).

Characteristic of Wave Deep Water Region to Shallow Water Region Shallow Water Region to Deep Water Region
Angle of incidence (\(i\)) and angle of refraction (\(r\)) Angle of incidence > angle of refraction (\(i > r\)) Angle of incidence < angle of refraction (\(i < r\))
Wavelength (\(\lambda\)) Decreasing (\(\lambda_2 < \lambda_1\)) Increasing (\(\lambda_2 > \lambda_1\))
Frequency (\(f\)) No change (constant, determined by vibration source) No change (constant, determined by vibration source)
Wave speed (\(v\)) Decreasing (\(v_2 < v_1\)) Increasing (\(v_2 > v_1\))
Direction of propagation Refracted towards the normal Refracted away from the normal

Steps to Draw Refraction Diagrams

Step 1: Draw an arrowed line \(AB\) perpendicular to the incident wavefronts to represent the direction of propagation of the incident wave.

Step 2: Draw the normal line perpendicular to the boundary between the deep and shallow regions at point \(B\).

Step 3: Draw an arrowed line \(BC\) representing the refracted ray. From deep to shallow, \(BC\) is bent nearer/towards the normal than \(AB\). From shallow to deep, \(BC\) is bent away from the normal.

Step 4: Draw parallel lines perpendicular to line \(BC\) to represent the refracted wavefronts. For deep to shallow, refracted wavefront lines are drawn closer together. For shallow to deep, refracted wavefront lines are drawn farther apart.

Natural Phenomena

Sound during day: Air closer to Earth's surface is hotter than the cooler air above. Sound travels faster in hot air than in cold air. Sound waves are refracted upwards, away from the ground. Sound is heard weaker and less clearly by an observer on the ground.

Sound at night: Air closer to Earth's surface is colder than the warmer air above. Sound travels slower near the ground and faster in the warmer upper layer. Sound waves are refracted downwards, towards the ground. Sound is heard louder and more clearly by an observer on the ground.

Sea waves at shoreline: Capes are shallow water regions, while bays are deeper water regions. Wave energy converges towards the cape, causing higher waves. Wave energy diverges away from the bay, causing calmer water with smaller amplitude waves.

Try to Answer First

Answer in your mind, then press “Check Answer”.

1

What wave characteristic remains unchanged when a plane water wave is refracted from a deep region into a shallow region?

Check Answer
Answer: The frequency of the wave remains unchanged.
2

When a plane water wave propagates from a deep water region to a shallow water region at an angle of incidence of \(45^\circ\), how does the angle of refraction compare to \(45^\circ\), and in which direction does the wave bend?

Check Answer
Answer: The angle of refraction is less than \(45^\circ\) (\(r < i\)), and the wave is refracted towards the normal.
3

A water wave with a wavelength of \(4\text{ cm}\) moves at a speed of \(16\text{ cm s}^{-1}\) in deep water. What is its speed in shallow water where its wavelength decreases to \(2.5\text{ cm}\)?

Check Answer
Answer: Using \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\), \(\frac{16}{4} = \frac{v_2}{2.5} \implies v_2 = 4 \times 2.5 = 10\text{ cm s}^{-1}\).

Common Mistakes

  • !Assuming that wave frequency changes when a wave enters a new medium. Frequency is strictly determined by the vibration frequency of the source and remains constant.
  • !Drawing wavefronts parallel to the direction of wave propagation instead of perpendicular (\(90^\circ\)) to it.
  • !Drawing refracted wavefronts with wider spacing in shallow water. In shallow water, speed is lower, so wavelength must be shorter / closer together.
  • !Confusing the behaviour of sound during day and night: forgetting that sound travels faster in hot air than in cold air, so it bends upwards during the day and downwards at night.

Concept Misunderstandings

Misunderstanding

Refraction only occurs if the wave hits the boundary at an angle.

Correct Concept

Speed and wavelength change whenever a wave enters a medium of different depth or optical density, even at normal incidence (\(i = 0^\circ\)). However, a change in the direction of propagation only occurs when the angle of incidence is greater than zero (\(i > 0^\circ\)).

Misunderstanding

Waves at bays have larger amplitude because bays are deeper.

Correct Concept

Wave energy converges at the capes (shallow water), resulting in higher wave amplitude. At bays, wave energy diverges and spreads over a wider area, resulting in smaller wave amplitude and calmer waters.

Summary

  • Refraction of waves is the change in propagation direction caused by a change in wave speed when crossing into a different medium or depth.
  • Deep \(\rightarrow\) Shallow: Speed decreases (\(v \downarrow\)), wavelength decreases (\(\lambda \downarrow\)), ray bends towards normal (\(i > r\)), frequency (\(f\)) remains constant.
  • Shallow \(\rightarrow\) Deep: Speed increases (\(v \uparrow\)), wavelength increases (\(\lambda \uparrow\)), ray bends away from normal (\(i < r\)), frequency (\(f\)) remains constant.
  • Calculations: Governed by the constant frequency relation \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\).
  • Applications/Phenomena: Day vs. Night sound: sound bends away from hot ground during day; bends towards cold ground at night. Shorelines: wave crests curve to match shore contours; waves converge at capes (higher amplitude) and diverge at bays (calmer, lower amplitude).

Short Activity

Objective: Test your understanding of wave refraction, wave characteristics and natural phenomena.

A. Objective Quiz

1 What happens to the wavelength and speed of a plane water wave when it propagates from a shallow region into a deep region?

2 Why can sound from a distant source be heard more clearly and louder at night than during the day?

B. Fill in the Blanks

3 During the refraction of waves, the property of the wave that remains completely unchanged across different media is its .

4 When sea waves approach the shoreline, wave energy converges towards the cape and diverges at the .

C. Matching / Drag and Drop

Drag each term to the correct meaning. If using a phone, tap the answer first, then tap the matching box.

Situation / Feature
Deep to shallow water
Shallow to deep water
Cape
Daytime sound propagation
Effect / Characteristic
Wave speed decreases and ray bends towards normalCorrect ✓Try againEmpty
Wave speed increases and ray bends away from normalCorrect ✓Try againEmpty
Shallow water region where wave energy converges, giving higher amplitudeCorrect ✓Try againEmpty
Sound travels faster near hot ground and refracts upwards into the airCorrect ✓Try againEmpty
 

Keywords

Refraction of waves Angle of incidence Angle of refraction Normal line Cape Bay Wavefront

Refraction of Waves

5.4 Refraction of Waves
PHYSICS • Form 4 • Chapter 5: Waves

5.4 Refraction of Waves

Refraction of waves is the change in the direction of propagation of waves caused by the change in the velocity of waves when propagating from one medium to another. In water waves, variations in water depth alter wave speed and wavelength, while the frequency remains unchanged. This concept explains natural occurrences such as sea waves curving to follow shorelines and sound being heard more clearly at night than during the day.

Learning Objectives

  • Define the refraction of waves.
  • Describe the effects of refraction on wave characteristics as waves travel between regions of different depths or media.
  • Draw and complete diagrams of refraction of plane water waves approaching a boundary at an angle.
  • Explain daily life and natural phenomena involving wave refraction.
  • Solve numerical problems involving wave refraction using \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\).

Refraction of Water Waves Across Depth Boundaries and Shorelines

See how wave direction, speed and wavelength change between deep and shallow regions, and how this relates to wave behaviour at capes and bays.

Deep to Shallow Water

Deep region Longer wavelength
Shallow region Shorter wavelength

Refraction at a Boundary

Deep waterShallow waterNormalIncident rayRefracted rayir

Short Explanation

What is Refraction of Waves?

Refraction of waves is the change in direction of propagation of waves caused by the change in the velocity of waves when the waves propagate from one medium to another.

Speed Dependencies

Speed of water waves is influenced by the depth of water. Speed of sound waves is influenced by the density of air. Speed of light waves is influenced by the optical density of the medium.

Key Relationship

Since frequency \(f\) remains constant during refraction: \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\) or \(\frac{v_1}{v_2} = \frac{\lambda_1}{\lambda_2}\).

Wave Speed Formula

Wave speed is given by \(v = f\lambda\), so \(f = \frac{v}{\lambda}\).

Characteristic of Wave Deep Water Region to Shallow Water Region Shallow Water Region to Deep Water Region
Angle of incidence (\(i\)) and angle of refraction (\(r\)) Angle of incidence > angle of refraction (\(i > r\)) Angle of incidence < angle of refraction (\(i < r\))
Wavelength (\(\lambda\)) Decreasing (\(\lambda_2 < \lambda_1\)) Increasing (\(\lambda_2 > \lambda_1\))
Frequency (\(f\)) No change (constant, determined by vibration source) No change (constant, determined by vibration source)
Wave speed (\(v\)) Decreasing (\(v_2 < v_1\)) Increasing (\(v_2 > v_1\))
Direction of propagation Refracted towards the normal Refracted away from the normal

Steps to Draw Refraction Diagrams

Step 1: Draw an arrowed line \(AB\) perpendicular to the incident wavefronts to represent the direction of propagation of the incident wave.

Step 2: Draw the normal line perpendicular to the boundary between the deep and shallow regions at point \(B\).

Step 3: Draw an arrowed line \(BC\) representing the refracted ray. From deep to shallow, \(BC\) is bent nearer/towards the normal than \(AB\). From shallow to deep, \(BC\) is bent away from the normal.

Step 4: Draw parallel lines perpendicular to line \(BC\) to represent the refracted wavefronts. For deep to shallow, refracted wavefront lines are drawn closer together. For shallow to deep, refracted wavefront lines are drawn farther apart.

Natural Phenomena

Sound during day: Air closer to Earth's surface is hotter than the cooler air above. Sound travels faster in hot air than in cold air. Sound waves are refracted upwards, away from the ground. Sound is heard weaker and less clearly by an observer on the ground.

Sound at night: Air closer to Earth's surface is colder than the warmer air above. Sound travels slower near the ground and faster in the warmer upper layer. Sound waves are refracted downwards, towards the ground. Sound is heard louder and more clearly by an observer on the ground.

Sea waves at shoreline: Capes are shallow water regions, while bays are deeper water regions. Wave energy converges towards the cape, causing higher waves. Wave energy diverges away from the bay, causing calmer water with smaller amplitude waves.

Try to Answer First

Answer in your mind, then press “Check Answer”.

1

What wave characteristic remains unchanged when a plane water wave is refracted from a deep region into a shallow region?

Check Answer
Answer: The frequency of the wave remains unchanged.
2

When a plane water wave propagates from a deep water region to a shallow water region at an angle of incidence of \(45^\circ\), how does the angle of refraction compare to \(45^\circ\), and in which direction does the wave bend?

Check Answer
Answer: The angle of refraction is less than \(45^\circ\) (\(r < i\)), and the wave is refracted towards the normal.
3

A water wave with a wavelength of \(4\text{ cm}\) moves at a speed of \(16\text{ cm s}^{-1}\) in deep water. What is its speed in shallow water where its wavelength decreases to \(2.5\text{ cm}\)?

Check Answer
Answer: Using \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\), \(\frac{16}{4} = \frac{v_2}{2.5} \implies v_2 = 4 \times 2.5 = 10\text{ cm s}^{-1}\).

Common Mistakes

  • !Assuming that wave frequency changes when a wave enters a new medium. Frequency is strictly determined by the vibration frequency of the source and remains constant.
  • !Drawing wavefronts parallel to the direction of wave propagation instead of perpendicular (\(90^\circ\)) to it.
  • !Drawing refracted wavefronts with wider spacing in shallow water. In shallow water, speed is lower, so wavelength must be shorter / closer together.
  • !Confusing the behaviour of sound during day and night: forgetting that sound travels faster in hot air than in cold air, so it bends upwards during the day and downwards at night.

Concept Misunderstandings

Misunderstanding

Refraction only occurs if the wave hits the boundary at an angle.

Correct Concept

Speed and wavelength change whenever a wave enters a medium of different depth or optical density, even at normal incidence (\(i = 0^\circ\)). However, a change in the direction of propagation only occurs when the angle of incidence is greater than zero (\(i > 0^\circ\)).

Misunderstanding

Waves at bays have larger amplitude because bays are deeper.

Correct Concept

Wave energy converges at the capes (shallow water), resulting in higher wave amplitude. At bays, wave energy diverges and spreads over a wider area, resulting in smaller wave amplitude and calmer waters.

Summary

  • Refraction of waves is the change in propagation direction caused by a change in wave speed when crossing into a different medium or depth.
  • Deep \(\rightarrow\) Shallow: Speed decreases (\(v \downarrow\)), wavelength decreases (\(\lambda \downarrow\)), ray bends towards normal (\(i > r\)), frequency (\(f\)) remains constant.
  • Shallow \(\rightarrow\) Deep: Speed increases (\(v \uparrow\)), wavelength increases (\(\lambda \uparrow\)), ray bends away from normal (\(i < r\)), frequency (\(f\)) remains constant.
  • Calculations: Governed by the constant frequency relation \(\frac{v_1}{\lambda_1} = \frac{v_2}{\lambda_2}\).
  • Applications/Phenomena: Day vs. Night sound: sound bends away from hot ground during day; bends towards cold ground at night. Shorelines: wave crests curve to match shore contours; waves converge at capes (higher amplitude) and diverge at bays (calmer, lower amplitude).

Short Activity

Objective: Test your understanding of wave refraction, wave characteristics and natural phenomena.

A. Objective Quiz

1 What happens to the wavelength and speed of a plane water wave when it propagates from a shallow region into a deep region?

2 Why can sound from a distant source be heard more clearly and louder at night than during the day?

B. Fill in the Blanks

3 During the refraction of waves, the property of the wave that remains completely unchanged across different media is its .

4 When sea waves approach the shoreline, wave energy converges towards the cape and diverges at the .

C. Matching / Drag and Drop

Drag each term to the correct meaning. If using a phone, tap the answer first, then tap the matching box.

Situation / Feature
Deep to shallow water
Shallow to deep water
Cape
Daytime sound propagation
Effect / Characteristic
Wave speed decreases and ray bends towards normalCorrect ✓Try againEmpty
Wave speed increases and ray bends away from normalCorrect ✓Try againEmpty
Shallow water region where wave energy converges, giving higher amplitudeCorrect ✓Try againEmpty
Sound travels faster near hot ground and refracts upwards into the airCorrect ✓Try againEmpty
 

Keywords

Refraction of waves Angle of incidence Angle of refraction Normal line Cape Bay Wavefront