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Mountain Lee Waves: Scorer Parameter, Trapped Waves, Lenticular Clouds and Wave Soaring

An exploration of atmospheric dynamics that reveals the physics behind soaring gliders and cloud formations.

mysimulator teamUpdated June 2026≈ 3 min read▶ Open the simulation

What Are Mountain Lee Waves?

Mountain lee waves are atmospheric waves that form on the downwind side of a mountain or hill as air flows over it. These waves can be observed as oscillations in temperature, pressure, and wind direction.

The formation of these waves is governed by the balance between the Coriolis force, gravity, and the vertical motion of air masses.

The Role of the Scorer Parameter

The Scorer parameter (S) is a dimensionless number that characterizes the stability of the atmosphere. It helps predict whether lee waves will form by comparing the Brunt-Väisälä frequency to the vertical wind shear.

A positive Scorer parameter indicates stable conditions, while a negative value suggests instability and wave formation.

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Trapped Waves and Their Impact

Trapped lee waves occur when the atmosphere is unstable and the wind speed increases with height. These waves are confined to the region near the mountain top and can lead to significant vertical motions.

The trapped nature of these waves makes them ideal for glider soaring, as they provide lift that gliders can use to climb without engine power.

Lenticular Clouds: A Visual Indicator

Lenticular clouds are lens-shaped clouds that form on the leeward side of mountains when moist air is forced to rise and cool, leading to condensation. These clouds are a clear visual indicator of lee wave activity.

The presence of lenticular clouds often signifies favorable conditions for glider soaring, as they indicate the presence of strong vertical motions in the atmosphere.

Frequently asked questions

What causes the Scorer parameter to change?

The Scorer parameter changes based on variations in atmospheric stability and wind shear. An increase in instability or a decrease in wind shear can lead to a more negative Scorer parameter, promoting wave formation.

How do lenticular clouds form during lee waves?

Lenticular clouds form when moist air is forced to rise and cool over the mountain. As the air cools, it reaches its dew point, causing water vapor to condense into cloud droplets.

Can lee waves be dangerous for aircraft?

Yes, lee waves can pose a risk to aircraft, especially those not designed for wave soaring. The strong vertical motions and turbulence associated with these waves can cause significant stress on the aircraft and may lead to loss of control.

How do gliders use lee waves for soaring?

Glider pilots use the updrafts created by lee waves to gain altitude without engine power. By flying at specific altitudes where the vertical motion is most favorable, gliders can harness these waves to extend their flight range and duration.

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Everything above runs in your browser — open Mountain Lee Waves: Scorer Parameter, Trapped Waves, Lenticular Clouds and Wave Soaring and change the parameters while it is running. Nothing is installed, nothing is uploaded, the whole model lives in one tab.

▶ Open Mountain Lee Waves: Scorer Parameter, Trapped Waves, Lenticular Clouds and Wave Soaring simulation

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