18.8 Raindrops and Refraction

Reflect on the Big Picture
Do refraction, total internal reflection, and dispersion support the wave model of light? The bending or refracting of light can be understood in terms of a transverse wave. Recall that the universal wave equation relates the speed, wavelength, and frequency of a transverse wave:
v = fλ
Consider a transverse light wave travelling from air into water. As the light wave enters the water, it slows down and the wavelength gets compressed. The frequency, however, remains unchanged, because the waves do not pile up at the boundary. The number of waves arriving at the boundary each second is equal to the number of waves leaving the boundary every second. Therefore, the frequency of the wave is constant as the wavelength shrinks. This helps us understand the change in speed when EMR is considered as a transverse wave. If the wavelength shrinks and the frequency remains constant, then the speed must also be reduced according to the universal wave equation.
As the wave fronts are compressed and slowed in the water, they change direction relative to the arriving, uncompressed, faster wave fronts still in the air. To visualize this in terms of wave fronts, imagine a line of 100 people all holding hands and running on the beach. If those runners closest to the water enter it and slow down, what happens to the shape of the line?

