Tag Archives: rogue waves

There’s no such thing as a freak wave – coastal safety is your own responsibility

I was reading a letter to Tramore Town Council, about the new Guillamenes cattle-crush, from someone who’d been involved in International Water Safety for many years. In the letter the person pointed out how someone had been “swept off the diving platform by a freak wave”. I said the Club Secretary Aidan Farrally that his points were valid but subsequent to that assertion, his arguments became suspect.

Now despite my deliberately somewhat provocative title, yes there are such things as freak waves. However while they are long reported, they are an only recently confirmed open ocean phenomenon, and more commonly known as rogue waves, (twice the height of the significant wave height around them).

But here we are discussing so-called freak waves at the coast, the interface of land and sea.

Every year we read or hear stories of coastal drownings caused by freak waves, where people at the coast are caught by a wave seemingly out of scale or size to the preceding waves, and swept off rocks, out to sea or suffering a fatal concussion from rocks. These are tragedies, but I have long had a problem with this reporting because it perpetuates a myth about the sea, and somewhat shifts the responsibility of care away from the person into a force-majeure situation, an “act of god“.

If there are freak waves, how can an average person realistically protect themselves except to stay away from the coast? If there aren’t freak waves, then the responsibility shifts to people themselves to be more vigilant.

The phrase freak wave implies that what has happened is unusual and unforeseen, neither of which are the case. Ask any surfer. So we need once again to talk about waves and safety at the coast.

Wind & WavesMost waves are caused by wind. Wind blows over the water surface and the friction pushes the water. The distance of water over which the wind blows is called the fetch, and the longer the fetch, and the longer the time and stronger the wind that blows, the bigger the initial waves. If the wind continues to blow, as the waves grow, they present even more surface for the wind to push. The waves continue to grow.

Waves are an energy pulse that travels through the water and will continue to travel unless something stops them. That something from our point of view, is land.

I said initial waves above, and that’s really important. Wind that blows in a Western Atlantic storm cause waves, which if unimpeded by other contrary weather, may blow those winds toward Ireland and Europe, across 2000 miles of open water. 

We need to think about the fundamentals of a wave.

Imagine the wind blowing and causing waves.

  • The height of a wave is called the amplitude.
  • The greater the amplitude the more energy in the wave.
  • The number of waves in a particular time is called the frequency.

Waves of different amplitudes usually have different frequencies. The higher the amplitude or height, the lower the frequency.

The bigger the wave, the longer the time between them and the less frequently they appear.

Waves travel at different speeds. Wind that cause waves nearby can have lots and lots of chop, small waves really close to each other.

Now the critical things about waves of any kind, not just water, is if they are even fractionally different heights they will travel at different speeds. What happens if two things, in case waves, are travelling the same direction at different speeds? The faster one will pass the slower one.

The further away the initial wind, the further the waves will travel. If a faster waves catches a slower one, the basic physics means that they will be added together. The amplitude, the height of the waves, will become the two combined heights.

A one and half metre wave catching a one metre wave, will become a two and half metre wave.

This wave, in surfer’s parlance, is called a Set Wave. Surfers don’t see them as freaks, but as normal aspects of the ocean’s behaviour.

Set waves at Tramore pier
Long groundswell  waves at Tramore pier

This doesn’t happen quickly but when you have hundred or thousands of miles or kilometres in which it can happen, it doesn’t have to be quick.

Waves reaching Hawaii from the Aleutian Islands
Waves reaching Hawaii from the Aleutian Islands

The result is that you have a wave that is now a third higher than the higher of the two previous waves. And that may be higher than all the surrounding waves. And the bigger it is the faster it’s travelling but the longer time between them, so there can up to many minutes between large waves like this. Any experienced surfer can tell you that the period between the largest set waves could be up to 15 minutes.

Now we’ve explored the formation and irregularity of waves, we’ve seen that these are not freak waves, but normal ocean behaviour.

The important thing becomes that the responsibility for understanding this lies with the person on the shore, just as it lies with a pedestrian crossing a road, except the ocean can’t see or react to you like a motorist can even when you are in the wrong.

Therefore the most important action to watch the water. Always.

This is NOT expect the unexpected. This is how the ocean works.

It should be noted, unlike beaches facing directly into the swell, at reefs and rocks, especially those that are not directly facing the oncoming swell, set waves can be difficult to see. if the water around a reef or rocky shore is deep, the first indication you may have is the wave actually breaking onto where you are standing

One wave seems to appear out of a flat surrounding sea at Tramore. easy to see on a beach, not easy to see elsewhere.
A wave seems to appear out of the flat surrounding sea at Tramore. Easy to see on a beach, not so easy to see elsewhere.

Watch the water for twice as long as the waves are high (in imperial measurement).

If the waves look to be two feet high, watch the water for four minutes before venturing close to the shore.

If the waves are two metres high on initial appraisal, you should (approximately) convert that to feet, and watch the water for six to seven minutes before getting close. Do this regularly and you will start to gain a better appreciation for the sea and its rhythms. And more importantly, you and the people around you will be safer.

Coastal safety is your responsibility!

Eagle island lighthouse-ireland_6787_600x450

Exploring freak waves

We’ve all heard (at least in Ireland) the unfortunate announcements of people losing their lives at the coast due to “freak waves”. Freak waves and rogue waves are the same thing, and are generally not what take unsuspecting people at the coast, since those are more generally set waves, which I’ve written about before, and people just don’t seem to understand that all waves around the same time are not the same size.

By the way, I’ll take this opportunity to remind you of the surfer’s saying to help ensure safety at the coast: watch the sea for twice as long as the waves are high.

Freak or rogue waves are the monsters that happen out to sea, that were long reported but generally not believed until very recently even though reports seemed to occur around the world. In Ireland the old lighthouse high up on Skellig Michael had its windows broken back in the 1950′s by waves breaking up at about 30 metres. On the 11th March 1861 at midday the lighthouse on Eagle Island, off the West coast of Ireland was struck by the sea smashing 23 panes, washing some of the lamps down the stairs, and damaging the reflectors with broken glass beyond repair. In order to damage the uppermost portion of the lighthouse, water would have had to surmount a seaside cliff measuring 40 m (133 ft) and a further 26 m (87 ft) of lighthouse structure.

VLCCs (very large cargo carriers) are notoriously lost going around Cape Horn (in the Agulhas Current), the theory is, being so long and heavy the wave can cause both ends of the ship to be suspended, (or the ends to be raised) and they break under their own unsupported weight.

In one those weird coincidences, when I was writing this, the M4 Buoy off Ireland’s North West registered a waves height of over 20 metres, truly extraordinarily large. I have seen 11 metre waves off Clare on the west coast, and, no word of lie, I remember looking out to sea and thinking to myself, I don’t remember there being an island there, before I realised what I was actually looking at. And then I went surfing.

Now the scientific and the orbital evidence (even you ignore reading and visuals) supports the existence of rogue waves after the measurement of The Draupner Wave, in 1995, (below). Here’s a scientific paper explaining the causal factors. There are a few factors, primarily high winds and strong currents.

I’m not sure if yesterday’s wave would qualify as rogue, since there were significant size waves before and after it. The strict(-ish) definition is that the wave is more than twice the significant height of the waves in the wave train, which wasn’t the case yesterday. But directly contradicting myself above, what the buoy did show was the wind blowing from the prevailing south-south-west direction. Rogue waves may occur when one wave travels in the opposite direction of the others and occur more frequently in areas with strong currents, such as the Agulhas off South Africa, the Kuroshio off Japan, and the Gulf Stream off the eastern United States. In 2000 a ship encountered an open water wave height of over 29 metres.

A Freak Wave took out the whole forepeaktank of the Norwegian tanker "Wilstar", 1974

Location is also important. VLCCs, which were too large to go through the Suez Canal have long had to take the long route to Europe around the Cape of Good Hope and some were mysteriously lost in the Agulhas Current. As many as 200 supertankers have been lost in the past 25 years, and many are now estimated to have been caused by freak waves with the SS Munchen being the best known. It also seems that the famous Edmund Fitzgerald may have been sunk by a peculiar freak wave phenomenon in Lake Superior!

A (short) YouTube clip of a collection of very large waves breaking at sea.

One scientist estimated there may be up to 10 of these waves in existence worldwide at any time, and in an important part of science, it’s been possible to recreate them in wave tanks, validating the science.