Wave Theory – And Practice, Part II


When we first put together the column on waves (see “Cat’s Paws to Grey Beards: Wave Theory – and Practice,”October 2012), I noted that we’d get back to waves and talk about different kinds of waves - tsunamis, deep, shallow, non-wind, etc. – and the effect they have on mariners. This column completes that promise.

Wind Creates Waves

Almost always, this is true. Almost. There are what scientists call “non-wind” waves; the two most common are the tides and tsunamis. Last month, I closed the column by noting that the longest wave on the planet was in fact that wave created by the Moon, lifting the water up and dragging it around the Earth. The closing question was, “What is the frequency?” The frequency of the tidal wave (not to be confused with a tsunami, often called a tidal wave) created by the rotation of the Moon around the Earth is about 12 ½ hours. The wavelength is half of the circumference of the Earth itself or roughly 12,451 miles. Looking at exhibit #1, you can easily see the representation of the wavelength.


Winds Create Waves

(exhibit #1 - courtesy: University of Arizona)

The tides themselves are divided into two types – Spring Tides, when the Earth, Moon and Sun align directly (higher highs, lower lows) and Neap Tides, when the Earth and Moon are at right-angles to the Sun and cancel somewhat the gravitational pulls (lower highs, higher lows.)


The tides are rarely dangerous, except to the skipper who doesn’t leave enough slack in his dock lines when making his boat fast to a fixed pier. But they are enormously powerful. How powerful? Over 80% of all the wave energy in the world is tied up in the tides. In fact, this energy and the friction related to it have actually lengthened the day on our planet. Over the past billion years, the day has lengthened from 19 hours to the present 24 hours.

What about what we called “tidal waves” as children – tsunamis? Traveling at speeds of 400 knots, tsunamis form in response to sudden changes in the shape and location of the sea floor, often due to landslides or earthquakes. Although devastating to affected areas, they are a small portion of the wave energy in the sea. Like any wave that breaks on the shore, these enormously high speed waves pile up at the water’s edge as all that energy compresses, much like a long train of train cars would pile up in an accident, rises up over itself and devastates all before it.

Wind DOES Create Waves

Jumping ahead since we’ve laid the groundwork back last month, take it as a given that the wind does create waves. And, on a windy but pleasant day, you can see the white caps marching in lock-step down the bays and in the offing to the ocean’s horizon. But many mariners have experienced “confused seas” where the waves seem to coming from everywhere, and typically these are foul weather seas. What is going on? The wind seems to be coming from one direction – but the waves aren’t. Why? This is due to the geometry of storms.

Most storms are low pressure systems, with cyclonic winds orbiting the storm center. The cyclonic wind field creates waves moving in every direction. These newly formed waves tend to be steeper and more severe and have shorter periods than waves outside of a generation area. After wind waves form, their growth is limited by the duration of energy input. Energy input is determined by the velocity, duration, and fetch of the wind field. Waves reach an equilibrium state (the “fully developed sea”) if all three of these variables remain constant for sufficient duration. For higher velocities, these conditions are rarely realized because the waves tend to run out of the area with high winds. Even in a hurricane 300 miles across, a typical large wave will move out of the source area within half a day, far too little time to allow development of a “full sea.”

So, there you have it. Wind creates waves – except for the longest wave, the tides, and the most destructive, the tsunami…

If you are interested in being part of USCG Forces, email me at JoinUSCGAux@aol.com or go direct to the D1SR Human Resources department, who are in charge of new members matters, at FSO-PS@emcg.us and we will help you “get in this thing.” F

Captain Joe Vojvodich is the Captain of the Port and Sector Commander for US Coast Guard Sector Long Island Sound. Captain Vojvodich is responsible for all active-duty, reservist and auxiliary Coast Guard personnel within the Sector. Vin Pica, Chief of Staff for the First District Southern Region in the US Coast Guard Auxiliary, works closely with Captain Vojvodich and his staff to promote boating safety in the waters between Connecticut, Long Island and 200 nautical miles offshore. Sector Long Island Sound Command Center can be reached 24 hours a day at 203-468-4401.

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