Page 334 - PPL-engelsk 2025
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Meteorology

                Mountain  waves  are  dangerous  because  they  cause  severe  turbulence  and

                unpredictable  updrafts

                and  downdrafts  on  the

                leeward  side,  which  can

                cause an aircraft to lose
                control.





                For mountain waves to form, the following conditions are required:

                  -  Stable air.

                  -  Wind direction nearly perpendicular to the mountain range—up to +/- 30
                      degrees.

                  -  Wind speed over the mountain top >25 knots.

                  -  Wind speed must increase with height above the mountain range.




                Mountain waves most commonly occur during the colder months of the year.

                The waves are stationary, and the air is lifted in front of the wave. If the air is

                moist enough, stationary clouds will form here due to adiabatic cooling.


                On the backside of the wave, the clouds will dissipate in the descending air.

                The clouds formed in connection with mountain waves are high Lenticularis

                clouds (lens-shaped clouds) and lower-laying rotor clouds.




                Rotor clouds form as a chain of CU-like clouds parallel to the mountain range

                on the leeward side beneath the wave crests. These clouds can grow into CB

                clouds with thunderstorms.

                On the windward side of the clouds, there are very strong updrafts, while there

                are downdrafts up to 5000 feet per minute on the leeward side.


                In and below the rotor cloud, there are areas with extremely strong turbulence.

                Updrafts and downdrafts of 1000 to 1500 feet per minute are not unusual.

                Along with the updrafts and downdrafts, there are also severe wind gusts.

                A  cap  cloud  forms  on  the  windward  side  of  the  mountain,  covering  the

                mountaintop and extending down the leeward side like a waterfall.
           Flight Theory PPL(A)(UL)/LAPL             Henning Andersen, Midtjysk Flyveskole© 2025           334
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