For the phenomenon of general relativity, see Gravitational wave.
Wave in or at the interface between fluids where gravity is the main equilibrium force
Nonfree image: detailed animation of a water wave
Detailed animation of water wave motion (CC-BY-NC-ND 4.0)
In fluid dynamics, gravity waves are waves generated in a fluid medium or at the interface between two media when the force of gravity or buoyancy tries to restore equilibrium. An example of such an interface is that between the atmosphere and the ocean, which gives rise to wind waves.
A gravity wave results when fluid is displaced from a position of equilibrium. The restoration of the fluid to equilibrium will produce a movement of the fluid back and forth, called a wave orbit.[1] Gravity waves on an air–sea interface of the ocean are called surface gravity waves (a type of surface wave), while gravity waves that are within the body of the water (such as between parts of different densities) are called internal waves. Wind-generated waves on the water surface are examples of gravity waves, as are tsunamis and ocean tides.
The period of wind-generated gravity waves on the free surface of the Earth's ponds, lakes, seas and oceans are predominantly between 0.3 and 30 seconds (corresponding to frequencies between 3 Hz and 30 mHz). Shorter waves are also affected by surface tension and are called gravity–capillary waves and (if hardly influenced by gravity) capillary waves. Alternatively, so-called infragravity waves, which are due to subharmonic nonlinear wave interaction with the wind waves, have periods longer than the accompanying wind-generated waves.[2]
^Lighthill, James (2001), Waves in fluids, Cambridge University Press, p. 205, ISBN 978-0-521-01045-0
^Bromirski, Peter D.; Sergienko, Olga V.; MacAyeal, Douglas R. (2010), "Transoceanic infragravity waves impacting Antarctic ice shelves", Geophysical Research Letters, 37 (L02502): n/a, Bibcode:2010GeoRL..37.2502B, doi:10.1029/2009GL041488, S2CID 38071443.
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connection with standing waves and even for random waves. The examples below describe Stokes waves under the action of gravity (without surface tension...
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another. Furthermore, time and size scales for gravitywaves and mammatus do not match up entirely. Gravitywave trains may be responsible for organizing the...
means that gravitational waves obey a massive wave equation and hence travel at speeds below the speed of light. Massive gravity has a long and winding...
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