Lee waves

Lee waves

In meteorology, lee waves, are atmospheric standing waves. The most common form is mountain waves, which are atmospheric internal gravity waves. These were discovered in 1933 by two German glider pilots, Hans Deutschmann and Wolf Hirth, above the Riesengebirge. [cite journal
title=Modeling and Classification of Mountain Waves
last=Tokgozlu
first=A
coauthors=Rasulov, M.; Aslan, Z.
year=2005
month=January
volume=29
issue=1
pages=p. 22
journal=Technical Soaring
issn=0744-8996
] [cite web
url = http://www.nateferguson.com/glider.html
title = Article about wave lift
accessdate = 2006-09-28
] They are periodic changes of atmospheric pressure, temperature and orthometric height in a current of air caused by vertical displacement, for example orographic lift when the wind blows over a mountain or mountain range. They can also be caused by the surface wind blowing over an escarpment or plateau, or even by upper winds deflected over a thermal updraft or cloud street.

The vertical motion forces periodic changes in speed and direction of the air within this air current. They always occur in groups on the lee side of the terrain that triggers them. Usually a turbulent horizontal vortex is generated around the first trough, the so called rotor. The strongest lee waves are produced when the lapse rate shows a stable layer above the obstruction, with an unstable layer above and below.cite book | last = Pagen | first = Dennis | title = Understanding the Sky | publisher = Sport Aviation Pubns | location = City | year = 1992 | isbn = 0936310103 | pages= pp.169-175 | quote= This is the ideal case, for an unstable layer below and above the stable layer create what can be described as a springboard for the stable layer to bounce on once the mountain begins the oscillation.]

Clouds

Both lee waves and the rotor may be indicated by specific wave cloud formations if there is sufficient moisture in the atmosphere, and sufficient vertical displacement to cool the air below the dew point. Waves may also form in dry air without cloud markers. Wave clouds do not move downwind as clouds usually do, but remain fixed in position relative to the obstruction that forms them.
* Around the crest of the wave, Adiabatic expansion cooling can form a cloud in shape of a lens (lenticularis). Multiple lenticular clouds can be stacked on top of each other if there are alternating layers of relatively dry and moist air aloft.
* The rotor may generate cumulus or cumulus fractus in its upwelling portion, also known as a "roll cloud". The rotor cloud looks like a line of cumulus. It forms on the lee side and parallel to the ridge line. Its base is near the height of the mountain peak, though the top can extend well above the peak and can merge with the lenticular clouds above. Rotor clouds have ragged leeward edges and are dangerously turbulent.
* A foehn wall cloud may exist at the lee side of the mountains, however this is not a reliable indication of the presence of lee waves.
* A Pileus or Cap Cloud, similar to a lenticular cloud, may form above the mountain or cumulus cloud generating the wave.
* Adiabatic compression heating in the trough of each wave oscillation may also evaporate cumulus or stratus clouds in the airmass, creating a "wave window" or "Foehn gap".ImageStackLeft|280

Aviation

Lee waves provide a possibility for gliders to gain altitude or fly long distances when soaring. World record wave flight performances for speed, distance or altitude have been made in the lee of the Sierra Nevada, Alps, Patagonic Andes, and Southern Alps mountain ranges. [ [http://records.fai.org/gliding/ FAI gliding records] ] The Perlan Project is working to demonstrate the viability of climbing above the tropopause in an unpowered glider using lee waves, making the transition into stratospheric standing waves. They did this for the first time on August 30, 2006 in Argentina, climbing to an altitude of 50,671 feet (15,447 m). [ [http://www.perlanproject.com/ Perlan Project] ] The Mountain Wave Project of the Organisation Scientifique et Technique du Vol à Voile focusses on analysis and classification of lee waves and associated rotors. [http://213.157.12.16/Defaultengl.htm Mountain Wave Project] - accessed 2008-02-17]

The conditions favoring strong lee waves suitable for soaring are:
* A gradual increase in windspeed with altitude
* Wind direction within 30° of perpendicular to the mountain ridgeline
* Strong low-altitude winds in a stable atmosphere
* Ridgetop winds of at least 20 knots

The rotor turbulence may be harmful for other small aircraft such as balloons, hang gliders and para gliders. It can even be a hazard for large aircraft; the phenomenon is believed responsible for many aviation accidents and incidents including the in-flight break up of BOAC Flight 911, a Boeing 707, near Mt. Fuji, Japan in 1966, and the in-flight separation of an engine on an Evergreen International Airlines Boeing 747 cargo jet near Anchorage, Alaska in 1993. [ [http://www.ntsb.gov/ntsb/brief.asp?ev_id=20001211X11963&key=1 NTSB Accident brief 20001211X11963] ]

The rising air of the wave, which allows gliders to climb to great heights, can also result in high altitude upset in jet aircraft trying to maintain level cruising flight in lee waves. Rising, descending or turbulent air in or above the lee waves can cause overspeed or stall, resulting in mach tuck and loss of control, especially when the aircraft is operated near the "coffin corner".

Other varieties of atmospheric waves

There are a variety of distinctive types of waves which form under different atmospheric conditions. Some less commonly known types are as follows:

* "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 distinguished by their towering roll clouds, and have been observed on the Sierra Nevada range [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] as well as mountain ranges in southern California.

* "Hydrostatic waves". These 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 waves" (or planetary waves) are large-scale motions in the atmosphere whose restoring force is the variation in Coriolis effect with latitude.

ee also

*Gravity wave
*Nor'west arch

References

Further reading

*Grimshaw, R., (2002). "Environmental Stratified Flows". Boston: Kluwer Academic Publishers.
*Jacobson, M., (1999). "Fundamentals of Atmospheric Modeling". Cambridge: Cambridge University Press.
*Nappo, C., (2002). "An Introduction to Atmospheric Gravity Waves". Boston: Academic Press.
*Pielke, R., (2002). "Mesoscale Meteorological Modeling". Boston: Academic Press.
*Turner, B., (1979). "Buoyancy Effects in Fluids". Cambridge: Cambridge University Press.
*Whiteman, C., (2000). "Mountain Meteorology". Oxford Oxfordshire: Oxford University Press.


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