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Additional recommended knowledge
When a fluid parcel is displaced on an interface or internally to a region with a different density, gravity restores the parcel toward equilibrium resulting in an oscillation about the equilibrium state. Gravity waves on an air-sea interface are called surface gravity waves or surface waves while internal gravity waves are called internal waves. Ocean waves and tsunamis are examples of gravity waves.
These waves are generated by wind in the oceans over areas known as the fetch. Gravity waves generally have a period of between 1 and 30 seconds (0.033 to 1 Hz). Alternatively, intragravity waves generally have a period between 30 seconds to 5 minutes (0.05 to 0.005 Hz). Infragravity waves can be felt rather than seen as they have a much greater wave energy.
Atmosphere dynamics on Earth
Since the fluid is a continuous medium, a traveling disturbance will result. In the earth's atmosphere, gravity waves are important for transferring momentum from the troposphere to the mesosphere. Gravity waves are generated in the troposphere by frontal systems or by airflow over mountains. At first waves propagate through the atmosphere without affecting its mean velocity. But as the waves reach more rarefied air at higher altitudes, their amplitude increases, and nonlinear effects cause the waves to break, transferring their momentum to the mean flow.
This process plays a key role in controlling the dynamics of the middle atmosphere.
The clouds in gravity waves can look like Altostratus undulatus clouds, and are sometimes confused with them, but the formation mechanism is different.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Gravity_wave". A list of authors is available in Wikipedia.|