Īlthough commonly described as a tsunami, the titular wave in The Great Wave off Kanagawa by Hokusai is more likely an example of a large rogue wave. Rogue holes have been replicated in experiments using water wave tanks, but have not been confirmed in the real world.

Ī 2012 study supported the existence of oceanic rogue holes, the inverse of rogue waves, where the depth of the hole can reach more than twice the significant wave height. They appear to be ubiquitous in nature and have also been reported in liquid helium, in quantum mechanics, in nonlinear optics, in microwave cavities, in Bose–Einstein condensation, in heat and diffusion, and in finance. Rogue waves can occur in media other than water. Rogue waves seem not to have a single distinct cause, but occur where physical factors such as high winds and strong currents cause waves to merge to create a single exceptionally large wave. Therefore, rogue waves are not necessarily the biggest waves found on the water they are, rather, unusually large waves for a given sea state. In oceanography, rogue waves are more precisely defined as waves whose height is more than twice the significant wave height ( H s or SWH), which is itself defined as the mean of the largest third of waves in a wave record. A rogue wave appearing at the shore is sometimes referred to as a sneaker wave.

They are distinct from tsunamis, which are often almost unnoticeable in deep waters and are caused by the displacement of water due to other phenomena (such as earthquakes). Rogue waves (also known as freak waves, monster waves, episodic waves, killer waves, extreme waves, and abnormal waves) are unusually large, unpredictable and suddenly appearing surface waves that can be extremely dangerous to ships, even to large ones. A merchant ship labouring in heavy seas as a large wave looms ahead, Bay of Biscay, ca.

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