Biographical Notes
The Earl E. Myers Story

Mountain Wave Information Attachment

Chapter 20
The Korean War And The Move To Yokota

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Mountain Wave Turbulence

In Australia, mountain waves and 'rotors' are commonly experienced over and to the lee of mountain ranges in the south-east of the continent. They often appear in the strong westerly wind flows on the east coast in late winter and early spring.

Mountain waves and 'rotors' are among the more hazardous phenomena aircraft can experience. Understanding the dynamics of the wind is important in improving aviation safety.

Glider pilots learn to use these mountain waves to their advantage however some aircraft have come to grief. Encounters have been described as similar to hitting a wall. In 1966, a mountain wave ripped apart a BOAC Boeing 707 while it flew near Mt. Fuji in Japan. In 1968, a Fairchild F-27B lost parts of its wings and empennage, and in 1992 a Douglas DC-8 lost an engine and wingtip in mountain wave encounters.

Mountain waves are the result of flowing air being forced to rise up the windward side of a mountain barrier, then as a result of certain atmospheric conditions, sinking down the leeward side. This 'bounce' forms a series of standing waves downstream from the barrier and may extend for hundreds of kilometres, which can be felt over clear areas of land and open water.

Formation of mountain waves relies on several conditions. The atmosphere is usually stable and an inversion may exist. The wind has to be blowing almost constantly within 30 degrees perpendicular to the barrier at a minimum speed of about 20 to 25 knots at the ridgeline. Wind speed increases uniformly with height and blows in the same direction. Wave 'crests' can be upwind or downwind from the mountain range and their amplitude seems to vary with the vertical stability of the flow. The crests of the waves may be identified by the formation of lens-shaped or lenticular clouds, depending on sufficient moisture in the air. Mountain waves may extend into the stratosphere and become more pronounced as height increases. Some pilots have reported mountain waves at 60,000 feet. The vertical airflow component of a standing wave may exceed 8,000 feet per minute.

Mountain wave turbulence
Graphic A

Mountain wave turbulence
Graphic B

Rotors or eddies can also be found embedded in mountain waves. Formation of rotors can also occur as a result of down slope winds. Their formation usually occurs where wind speeds change in a wave or where friction slows the wind near to the ground. Often these rotors will be experienced as gusts or windshear. Clouds may also form within a rotor.

Many dangers lie in the effects of mountain waves and rotors on aircraft performance and control. In addition to generating turbulence that has demonstrated sufficient ferocity to significantly damage aircraft or lead to loss of aircraft control, the more prevailing danger to aircraft in the lower levels in Australia seems to be the effect on the climb rate of an aircraft. General aviation aircraft rarely have performance capability sufficient to enable the pilot to overcome the effects of a severe downdraft generated by a mountain wave or the turbulence or windshear generated by a rotor. In 1996, three people were fatally injured when a Cessna 206 encountered lee (mountain) waves. The investigation report concluded, "It is probable that the maximum climb performance of the aircraft was not capable of overcoming the strong downdrafts in the area at the time".

Crossing a barrier into wind also reduces the groundspeed of an aircraft and has the effect of keeping the aircraft in the area of downdraft for longer. An aircraft flying downwind is likely to place an aircraft in an updraft as it approaches rising ground. Rotors and turbulence may also affect low level flying operations near hills or trees. In 1999, a Kawasaki KH-4 hit the surface of a lake during spraying operations at 30 feet. The lack of sufficient height to overcome the effects of wind eddies and turbulence was implicated as a factor involved in the accident.

Research into mountain waves and rotors or eddies continues but there is no doubt that pilots need to be aware of the phenomenon and take appropriate precautions. Although mountain wave activity is normally forecast many local factors may effect the formation of rotors and eddies. When planning a flight a pilot should take note of the winds and the terrain to assess the likelihood of waves and rotors. There may be telltale signs in flight, including the disturbances on water or wheat fields and the formation of clouds, provided there is sufficient humidity to provide for cloud formation.

Some considerations include allowing for the possibility of significant variations in the aircrafts altitude if up and downdraughts are encountered. A margin of at least the height of the hill or mountain from the surface should be allowed. Ultimately, it may be preferable for pilots to consider diverting or not flying, rather than risk flying near or over mountainous terrain in strong wind conditions conducive to mountain waves and rotors.

Further Reading

* Bureau of Meteorology. (1988). Manual of meteorology part 2: Aviation meteorology. Canberra, ACT: Australian Government Publishing Service.
* Bureau of Meteorology. (1991, September). Downslope winds are dangerous. BASI Journal, 9, 38-39.
* Jorgensen, K. (undated). Mountain flying: A guide to helicopter flying in mountainous and high altitude areas. Westcourt, QLD: Cranford Publications.
* Lester, P. F. (1993). Turbulence: A new perspective for pilots. Englewood, CO: Jeppesen Sanderson.
* Welch, John, F. (Ed.). (1995). Van Sickles modern airmanship (7th Ed). New York, NY: McGraw-Hill.
* Woods, R. H., & Sweginnis, R. W. (1995). Aircraft accident investigation. Casper, WY: Endeavor Books.

End of Mountain Wave Information

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