When approaching a mountain ridge, it is advantageous, if heading upwind towards it, to cross at an angle of around 30 - 45 degrees in order to allow an escape should downdrafts prove excessive.
In the Alps regions, particularly in the Zurich – Milano regions, a general rule of thumb that a QNH difference of more than 5 – 8 mb between LSZH and LIMC, for example, or between north and south of the Alps, will provide for significant mountain wave activity over the Alps. A higher QNH in Zurich will result in mountain waves south of the Alps, for example.
If significant mountain wave activity is expected, as a rule of thumb and if possible plan a flight at least 5000 – 8000 feet above the highest elevation along your route.
Local knowledge of the conditions which tend to cause the formation of mountain waves enables forecasting of potential wave propagation.
Lenticular Clouds (lens shaped clouds) can form in the crest of the mountain waves if the air is moist. Roll Clouds can also occur in the rotors below the waves if the air is moist. These clouds are a good indication of the presence of mountain waves but, if the air is dry, there may not be any cloud to see. Windward of the mountains IMC conditions may likely be present, whereas due to the “Foehn Effect” VMC conditions are generally expected to the leeward.
Passengers and flight crew should routinely wear their seat belts / harnesses when seated to provide protection against unexpected turbulence.