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Gravity wave information


Surface gravity wave, breaking on an ocean beach in Tučepi, Croatia
Wave clouds over Theresa, Wisconsin, United States
Nonfree image: detailed animation of a water wave
image icon Detailed animation of water wave motion (CC-BY-NC-ND 4.0)
wave clouds observed over the ocean, seen from a satellite
Atmospheric gravity waves at Shark Bay, Western Australia, Australia as seen from space

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]

  1. ^ Lighthill, James (2001), Waves in fluids, Cambridge University Press, p. 205, ISBN 978-0-521-01045-0
  2. ^ 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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