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A gravity wave in oceanography is a wave on the surface of water where gravity acts as the restoring force, tending to flatten the surface. These waves are distinct from ripples, which are driven by surface tension.12

Gravity waves in the ocean are typically longer than approximately 10 cm (4 inches). Their speed is influenced by water depth and wavelength; longer waves and deeper water generally lead to faster speeds. Wind is the primary generator of these waves, and after the wind subsides, they can continue to propagate as swell.2

Internal waves are another type of gravity wave that occur within the ocean, at boundaries between water layers of different densities. These internal waves move much slower than surface gravity waves.3

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