Editing Lee wave (section)

==Other varieties of atmospheric waves==
[[File:Hydrostatic.JPG|thumb|Hydrostatic wave (schematic drawing)]]

There are a variety of distinctive types of waves which form under different atmospheric conditions.

* ''[[Wind shear]]'' can also create waves. This occurs when an [[atmospheric inversion]] separates two layers with a marked difference in wind direction. If the wind encounters distortions in the inversion layer caused by [[thermal]]s coming up from below, it will create significant shear waves in the lee of the distortions that can be used for soaring.<ref>{{cite book
|last = Eckey
|first = Bernard
|title = Advanced Soaring Made Easy
|publisher = Eqip Verbung & Verlag GmbH
|year = 2007
|isbn = 978-3-9808838-2-5
}}</ref>

* ''Hydraulic jump induced waves'' are a type of wave that forms when there exists a lower layer of air which is dense, yet thin relative to the size of the mountain.  After flowing over the mountain, a type of shock wave forms at the trough of the flow, and a sharp vertical discontinuity called the [[hydraulic jump]] forms which can be several times higher than the mountain.  The hydraulic jump is similar to a rotor in that it is very turbulent, yet it is not as spatially localized as a rotor.  The hydraulic jump itself acts as an obstruction for the stable layer of air moving above it, thereby triggering wave.  Hydraulic jumps can be distinguished by their towering roll clouds, and have been observed on the [[Sierra Nevada (U.S.)|Sierra Nevada]] range<ref name="Kuettner+Hertenstein">[http://ams.confex.com/ams/pdfpapers/40363.pdf Observations of Mountain-Induced Rotors and Related Hypotheses: a Review] by Joachim Kuettner and Rolf F. Hertenstein</ref> as well as mountain ranges in southern California.
* ''Hydrostatic waves'' are vertically propagating waves which form over spatially large obstructions.  In hydrostatic equilibrium, the pressure of a fluid can depend only on altitude, not on horizontal displacement.  Hydrostatic waves get their name from the fact that they approximately obey the laws of hydrostatics, i.e. pressure amplitudes vary primarily in the vertical direction instead of the horizontal.  Whereas conventional, non-hydrostatic waves are characterized by horizontal undulations of lift and sink, largely independent of altitude, hydrostatic waves are characterized by undulations of lift and sink at different altitudes over the same ground position.
* ''[[Kelvin–Helmholtz instability]]'' can occur when velocity shear is present within a continuous fluid or when there is sufficient velocity difference across the interface between two fluids.
* ''[[Rossby wave]]s'' (or planetary waves) are large-scale motions in the atmosphere whose restoring force is the variation in Coriolis effect with latitude.