Early in the morning on Sept. 11, 1995, the cruise liner the Queen Elizabeth 2, on its way from Southampton to New York, was being lashed by the tail end of Hurricane Luis, somewhere off the coast of Newfoundland. As if sensing its imminent demise, Luis had galvanized one last time, twitching to life and whipping the North Atlantic into a torrent of 130 mph winds and 40-foot waves. None of this caused undue concern for the ship’s captain, Ronald Warwick, a 30-year sailing veteran well acquainted with rough seas. Luis was hardly unexpected; since leaving England, the ship had steadily tracked the storm’s path. “This was fair game for us,” the retired Commodore recalls, from his home in Somerset, England. “We are a transatlantic liner.”
At dinner, Warwick had advised the ship’s passengers that things might get a bit rough during the night, and to secure any loose possessions in their cabin. He then did what any captain would do in heavy seas. With the ship steered into the waves, Warwick slowed it to a few knots. “Heaving to” it is called, the idea being to ride out the waves as gently as possible, while maintaining just enough speed to maintain steering control. Far below the ship’s bridge, where winds roared and whipped against the armored windows, a handful of passengers held casual vigil in a bar.
Just after 2 a.m., Warwick and his officers suddenly saw a surging monster of water and convulsive white froth in the near distance. “If you’re standing on the bridge of the QE2,” he says, “your height of eye above sea level is 90 feet.” From what they could discern through the rain-soaked darkness, the crest of the looming wave was as high as the bridge itself. Warwick, who says he had never encountered anything so large in the ocean before, said it was as if they were heading into the “white cliffs of Dover.”
The anomalousness of this one wave still haunts Warwick.
A minute or so later, the wave crashed across the forward deck of the QE2. “We didn’t go over the top of it,” says Warwick. “We virtually went through it.” A series of judders shot through the ship. The wall of water crashed down on the ship’s deck, buckling its steel plates some 18 inches. Still, this was all within the operating bounds of the ship. “We weren’t knocked off our feet or anything,” he says. “Most passengers were in bed.”
But the anomalousness of this one wave still haunts Warwick. For an old North Sea hand, 40-foot waves, the kind that would terrify most of us, were nothing out of the ordinary. But the emergence from nowhere of a single wave that was more than twice as high as the others was exceptional. Warwick had encountered a rogue wave.
In the common parlance, “rogue wave” has come to mean any wave that is unusually large. But a rogue wave does not have to be big on an absolute scale, nor is it necessarily associated with a heavy storm. Burkard Baschek, director of the Institute of Coastal Research, in Geesthacht, Germany, defines it as any wave that is statistically extreme. “[A rogue wave is] at least twice as high as the so-called significant wave height,” he says. The significant wave height is defined as the average of the largest one-third of waves at any given moment, “the waves you would see by eye if you’re out there and looking at the sea state.”
This means you have probably experienced a rogue wave and not noticed. How? “If you’re out in calm conditions,” says Baschek, “and the waves are one meter high, and suddenly you experience a two meter wave, so what?” In fact, Baschek says one wave per day, somewhere in the world’s oceans, is a rogue wave. While at the University of California, Los Angeles (UCLA), he analyzed data from a number of buoys off the west coast of the United States and, extrapolating the figures globally, estimated that ships trawling the North Atlantic (like the QE2) would “encounter 20-30 of these rogue waves during their service lives of 25 years,” or about one a year.
That rogue waves are, at base, mathematical objects has meant that sailors, then scientists, have been slow to grasp their nature. Late into the 19th century, the line between sailors’ lore and science could be as blurred as a fog-bound horizon, with reputable journals routinely reporting on the sightings of “monsters of the sea.” By the mid-20th century, though, most of these monsters had been dispelled or explained—but not rogue waves, which continue to be misidentified and incompletely understood today. Even one of civilization’s most famous waves, Hokusai’s The Great Wave off Kanagawa, is often misinterpreted as a tsunami—the woodcut has even been used as the symbol of a UNESCO tsunami warning sign—when it is actually more likely a rogue wave, as several scholars have argued.1,2
The science of rogue waves began to take shape in the early 1960s, not in the ocean but in a wave tank—essentially a long, shallow trough with a “paddle” for generating waves of varying frequencies—in Cambridge University’s Engineering Department. There, the physicist and fluid dynamics expert T. Brooke Benjamin, aided by a graduate student named Jim Feir, were having trouble trying to prove something that had long been assumed: the stability of the so-called “Stokes wave,” the sort of Ur-wave, or prototypical wave, of fluid dynamics, theorized by the renowned 19th-century Cambridge University mathematician George Gabriel Stokes. Stokes, inspired by a British engineer’s faintly astonished report of a “solitary heap of water,” pushed along by a slowing boat, that had maintained its speed and shape for nearly two miles as it traveled through a canal, looked for an equation that could describe a wave propagating in shallow water without changing shape.3
It had been rather taken for granted that the Stokes “wave trains,” as they were called, were essentially stable. But engineers working in wave tanks — testing ships’ hydrodynamics and the like—were finding instabilities.4 As they set out in their own search of stability, Feir and Benjamin noticed something odd. Their colleague, J.C.R. Hunt, wrote that the two “observed how waves generated at the wave maker started as a regular train with constant frequency and wavelength, but then about 5 m down the tank began to form into groups of waves with varying frequencies and wavelengths.”5 Thinking it might be a problem with the wave generating hardware, they first worked out a solution to keep the frequency from shifting. They then moved to a larger tank, with a programmable wave maker. But the results were the same. As the wave moved down the tank, it was buffeted by “sidebands” of higher and lower frequency. Critically, these sidebands grew exponentially in amplitude, or height, as they traveled down the tank.
The effect, now known as the “Benjamin-Feir instability,” offered a hint as to how rogue waves form. As J.B. Zirker describes in his book, The Science of Ocean Waves, the wave group, once it found a kind of sweet spot of modulation, stole energy from itself to produce a single high wave—higher than might be expected from the normal dynamics of the waves—then “returned” it to the primary wave. “The sidebands grew exponentially in height at the expense of the primary wave, which eventually disintegrated,” he writes. “Nobody had ever seen or expected the likes of this before.”
What ultimately made the concept of rogue waves so striking was not simply that they could grow to unexpected heights, but that they occurred more frequently than they were expected to. As Eric Heller, a physicist at Harvard University, explains it, much of the thinking on large wave creation was influenced by M.S. Longuet-Higgins, the noted mathematician and oceanographer, who was, as he wrote in one study, trying to “study theoretically the statistical properties of a random, moving Gaussian surface.” In other words, the ocean.
“His theory was based on the random addition of waves,” Heller says. “He was uniformly adding them up over large areas and asking how many unlucky additions you would get resulting in large waves.” It was a linear process. According to Heller, there was just one problem: “There were more freak wave events [in reality] than that theory could ever really account for. Light bulbs went off in people’s heads—it must be nonlinear evolution!”
And so rogue waves crashed into the longstanding “Gaussian seas” model of randomly distributed wave heights. They were not quite as long-tail as had been thought, and new probabilities, like the so-called “Tayfun distribution” (which coincidentally sounds like “typhoon” but is named for a Turkish scholar) have gained currency to predict the likelihood of rogue waves.
One of the biggest boons to the study of rogue waves came not in the laboratory, but in the ocean itself. On the night in 1995 that the QE2 was struck by the giant wave, there was another witness, one who experienced the wave from a deeply immersive position: “Buoy 44139,” an instrumented floating beacon monitored by the Canadian Forces Meteorological Office at Halifax. The statistical graph it generated during the torment is simple, yet chilling. There is a slightly jagged saw-tooth line of wave heights, the 40-foot rollers that Warwick had hove to against. But then, with no anticipatory buildup, there rises a single, dramatic peak, leaping toward the top of the page, almost, literally, “off the charts.” Just as suddenly, it plunges again, as if it were never there.
Buoys like 44139, equipped with accelerometers and other measuring devices, brought precision to an arena where sailor’s accounts and estimations had dominated. Before their advent, gauging the heights of waves was an inexact process. One early, and complicated, effort involved photographing the ocean from an airplane and mathematically estimating wave height via the reflection of light.6
But buoys are far from perfect. They get overtopped by waves, or knocked on their sides. There is also an issue of selection bias. Most instrumented buoys are located close to shore, says Baschek, while the largest rogue waves occur more frequently on the open ocean. Not all buoys can measure the direction of waves. And the big wave measurements that have been captured—the QE2, or, in another well-known instance earlier that same year, a 30-meter wave captured on the oil platform Draupner off the coast of Norway—are single point measurements. “It’s a buoy or a radar point,” he says. “But you have no idea what the crest length is. If you measure a rogue wave, is it one local spray, or is it going over miles and miles? How long does it persist? Does this rogue wave form right before your buoy and fall apart right after that? This is also something you don’t know.”
One of civilization’s most famous waves is often misinterpreted as a tsunami.
As a striking reminder of how science, even with its ever more sophisticated and powerful measurement capabilities, is still catching up with the enormity of the ocean, it was only in 2011 that the long-suspected, but never observed, phenomena of “merging tsunami”—two waves (formed non-linearly) becoming (linearly) a more powerful one—was finally observed in the wild, thanks to a procession of satellites orbiting over the tsunami. The capture of the merging tsunami was a “one in 10 million chance” random observation, as an investigator put it.7
For these reasons, even in this age of networked data and supercomputer simulations, some of the best data on rogue waves continues to come from the men and women who work on the sea.
In January, 2010, the crab boat Early Dawn (featured, as it happens, in the Deadliest Catch reality series), operating near the town of St. Paul, Alaska, was struck by a wave that was said to be twice as high as the significant wave height…
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Tom Vanderbilt writes on design, technology, science, and culture, among other subjects.
1. Cartwright, J.H.E. & Nakamura, N. What Kind of a Wave is Hokusai’s Great Wave Off Kanagawa. Notes and Records: The Royal Society Journal of the History of Science 63, 119–135 (2009).
2. Dudley, J.M., Sarano, V., & Dias, F. “On Hokusai’s Great Wave Off Kanagawa: Localization, linearity and a rogue wave in sub-Antarctic Waters. Notes and Records: The Royal Society Journal of the History of Science 67, 159-164 (2013).
3. Zirker, J.B. The Science of Ocean Waves Johns Hopkins University Press (2013).
4. Drazin, P.G. & Reid, W.H. Hydrodynamic Stability Cambridge University Press (2004).
5. Hunt, J.C.R. Nonlinear and Wave Theory Contributions of T. Brooke Benjamin (1929-1995) Annual Review of Fluid Mechanics 38, 1-25 (2006).
6. Jahne, B., Schmidt, M., & Rocholz, R. Combined optical slope/height measurements of short wind waves: principle and calibration. Measurement Science and Technology 16, 1937-1944 (2005).
7. Buis, A. & Cole, S. NASA finds Japan tsunami waves merged, doubling power. NASA.gov (2011).
8. Broderick, N. Viewpoint: Optical rogue waves on demand. Physics 3, 101 (2010).
*Due to an editorial error, this caption misspelled Nail Akhmediev’s first name as originally published.