Download Boating Tip #56: Waves (PDF format, 94KB)
Ocean waves are wind generated, with the exception of tsunami which are a result of seismic activity such as earthquakes, and volcanic eruptions. The effect that wind will have on wave formation depends on the wind speed, the duration or amount of time the wind blows over an area, and its fetch. The fetch is the unobstructed distance over which the wind blows. When waves travel beyond the fetch, the wavelength, period and direction of travel become more uniform, and the seas are then referred to as swell. Waves exists as energy as the swell moves through the water. Water doesn’t move in open oceans and lakes, although the opposite is true in rivers.
Capillary waves or ripples form first. As the size of a wave increases, it becomes narrower and steeper, developing the trochoid form unique to ocean waves.
Wave height (the vertical distance from the trough to the crest) is equal to 1/20th of the wave length (the horizontal distance from crest to crest). Wave motion is circular, with the circles getting progressively smaller as you go deeper in the water.
The pattern changes as the wave approaches shore. The ocean bottom crowds the energy upward, motion becomes oval shaped or elliptical rather than circular, and actually flat on the ocean bottom, surging forward and back.
When water depth equals one half of the wave length, the bottom friction begins to slow the advancing wave. The back of the wave crowds the front of the wave and water piles up. The bottom of the wave is moving slower than the top of the wave, so the top begins to curl. A wave will break , creating surf, when the angle at the crest falls below 120°, or when the height of the wave is 1/7th the length of the wave, or when wave height reaches 3/4 of the water depth.
The speed at which a wave travels in open water depends on its wavelength, and can be calculated using the formulas:
Speed (in knots) equals 3 times the interval period (in seconds)
____ C = 3 x T
or
Speed (in knots) equals 1.34 times the square root of the wavelength (in feet)
____ C = 1.34 V λ
T (Period) | λ (Wavelength) | C (Speed) |
6 seconds | 182 feet | 18 knots |
7 seconds | 242 feet | 21 knots |
8 seconds | 322 feet | 24 knots |
9 seconds | 408 feet | 27 knots |
10 seconds | 502 feet | 30 knots |
11 seconds | 610 feet | 33 knots |
12 seconds | 725 feet | 36 knots |
13 seconds | 850 feet | 39 knots |
14 seconds | 985 feet | 42 knots |
15 seconds | 1,128 feet | 45 knots |
16 seconds | 1,284 feet | 48 knots |
When waves move toward shallower water, wave speed decreases, the wavelengthbecomes shorter and height increases. Wave speed in shallow water is more dependant onthe depth of the water, and can be calculated using the formula:
Speed (in knots) equals 3.4 times the square root of the water depth (in feet)
____ C = 3.4 V h
h (Depth) | C (Speed) |
1 foot | 3.4 knots |
2 feet | 4.8 knots |
3 feet | 5.9 knots |
4 feet | 6.8 knots |
5 feet | 7.6 knots |
6 feet | 8.3 knots |
7 feet | 9.0 knots |
8 feet | 9.6 knots |
9 feet | 10.2 knots |
10 feet | 10.7 knots |
11 feet | 11.2 knots |
12 feet | 11.7 knots |
13 feet | 12.2 knots |
14 feet | 12.7 knots |
15 feet | 13.1 knots |
16 feet | 13.6 knots |
17 feet | 14.0 knots |
18 feet | 14.4 knots |
19 feet | 14.8 knots |
20 feet | 15.2 knots |
21 feet | 15.6 knots |
22 feet | 15.9 knots |
23 feet | 16.3 knots |
24 feet | 16.6 knots |
25 feet | 17.0 knots |
50 feet | 24.0 knots |
75 feet | 29.4 knots |
100 feet | 34.0 knots |
125 feet | 38.0 knots |
150 feet | 41.6 knots |
175 feet | 45.0 knots |
200 feet | 48.0 knots |