Opening page of the optional Mountain-Wave & Turbulence program module.
MOUNTAIN WAVES and WAVE TURBULENCE.
Wave Turbulence Overview.
This is an optional program module.
The RAOB program is the only commercially available sounding analyses program that produces mountain (lee) wave turbulence analyses. Even though RAOB also produces standard CAT and High Altitude CAT analyses, these forms of turbulence only use wind shear and lapse rates (respectively) as determining factors. Wave turbulence, however, is dependent on both wind speed and lapse rate in addition to terrain. In fact, results show that just the slightest variations in surface terrain can produce wave turbulence when the necessary wind shear and stability conditions are present – and the RAOB program has algorithms that objectively measure their combined effect upon the atmosphere.
There are literally hundreds of published articles on various mathematical solutions for wave turbulence, many of which have specific boundary conditions such as limited atmospheric layers or require explicit atmospheric lapse rates, wind shears, and terrain shapes. RAOB, on the other hand, consistently produces reasonable wave turbulence analyses using everyday soundings with user-definable mountain parameters, and without restriction to lapse rates or wind shear. Even though RAOB has a default mountain range parameter algorithm that will always produce a maximum wave scenario, it is absolutely essential that the user provide RAOB with actual mountain parameters in order to produce the best possible wave turbulence results for any individual sounding. This necessity is discussed in more detail in the following pages of this section.
All mathematics used by RAOB to
produce wave turbulence are taken from widely
acknowledged and quoted sources of wave turbulence theory (which are detailed
in the following pages). These theories
were developed before the age of computers and no applications algorithms
existed until
The author of RAOB has obtained Mr. Cale’s
wave turbulence algorithms and incorporated them into the RAOB program in an
interactive format. These algorithms
were independently validated and tested before acceptance into the RAOB
program. Test results were
remarkable. Very good correlations were
noted between soundings and reported wave activity. The author even found good correlation of
observed low-level wave induced clouds over the mid-western
It is important to note that even though RAOB consistently produces reasonable wave turbulence results, nearly all mountain and lee wave source documents indicate that there is no single set of equations that can accurately explain all wave phenomena. Furthermore, even though RAOB uses three parameters to define terrain (height, half-width, and ridge axis orientation), mountain shapes are much more complex than these simple definitions may suggest. In the meantime, improved and new methods are being sought for use in RAOB.
For those that require a complete analysis of atmospheric turbulence (with or without local terrain influences), RAOB’s Turbulence & Mountain-Wave module is must have tool