Waves on the ocean have wavelengths comparable to those of waves in seismic prospecting (15-500 meters), but ocean waves move slowly enough to be seen. Imagine a long harbor barrier parallel to the beach with a small entrance in the barrier for the passage of ships. This is shown in Figure 1.

Figure 1

A plane wave incident on the barrier from the open ocean will send a wave through the gap in the barrier. It is an observed fact that the wavefront in the harbor becomes a circle with the gap as its center. The difference between this beam of water waves and a light beam through a window is in the ratio of wavelength to hole size.

Linearity is a property of all low-amplitude waves (not those foamy, breaking waves near the shore). This means that two gaps in the harbor barrier make two semicircular wavefronts. Where the circles cross, the wave heights combine by simple linear addition. It is interesting to think of a barrier with many holes. In the limiting case of very many holes, the barrier disappears, being nothing but one gap alongside another. Semicircular wavefronts combine to make only the incident plane wave. Hyperbolas do the same. Figure 2 shows hyperbolas increasing in density from left to right.

Figure 2

All those waves at nonvertical angles must somehow combine with one another to extinguish all evidence of anything but the plane wave.

A Cartesian coordinate system has been superimposed
on the ocean surface with *x* going along the beach
and *z* measuring the distance from shore.
For the analogy with reflection seismology,
people are confined to the
beach (the earth's surface) where they make
measurements of wave height as a function of *x* and *t*.
From this data they can make inferences about
the existence of gaps in the barrier out in the (*x* , *z*)-plane.
The first frame of
Figure 3 shows the arrival time at the beach
of a wave from the ocean through a gap.

Figure 3

The earliest arrival occurs nearest the gap.
What mathematical expression determines
the shape of the arrival curve seen in the (*x* , *t*)-plane?

The waves are expanding circles.
An equation for a circle expanding with velocity *v* about
a point ( *x _{3}* ,

(1) |

If the original incident wave was a positive pulse,
the Huygens secondary source must consist of both positive
and negative polarities to enable the destructive
interference of all but the plane wave.
So the Huygens waveform has a phase shift.
In the next section,
mathematical expressions will be found for the Huygens secondary source.
Another phenomenon, well known to boaters,
is that the largest amplitude of the Huygens semicircle
is in the direction pointing straight toward shore.
The amplitude drops to zero for waves moving parallel to the shore.
In optics this amplitude drop-off with angle is called the
*
obliquity factor.
*

12/26/2000