Why use a term with a clear meaning like ‘terrain-induced’ when you can use something obscure like ‘orographic’? Well, you can save four letters and a hyphen and break brains in the process. Bonus!
Ororgraphic means ‘related to mountains’ and comes from the Greek word for hill, ‘oros’. Air moving over mountains is pushed up and over by the terrain, creating different clouds as it is forced up, on top, and coming down the other side. Here in Boulder Colorado we have a great view of clouds generated above the Rocky Mountains to the west of us. In the summer, the atmosphere is mostly unstable, and the upwards push of the mountains triggers thunderstorms that develop any time the air is moist enough. This often happens in mid to late summer, and we call this our ‘monsoon’. Thunderstorms form over the mountains, and then move out to the east, over the plains.
At other times of year, when the air is stable, we get very different clouds, most notably the altocumulus standing lenticularis (ACSL) , as shown in Figure 1. Lenticularis refers to the ‘lens’ or ‘lentil’ shape. This cloud is also known as a ‘mountain wave’ cloud. When the air is stable, and wind comes from the west across the Rockies, it can overshoot as it comes down, descending below the optimum altitude for its density. Like a spring-mass-damper system, it essentially bounces back up, overshooting again by going too high. The bounce repeats, often in a diminishing series of bounces, like ripples on a pond, also known as gravity waves – these are common here on Earth, unlike Einstein’s gravitational waves . At the top of each bounce, the air is cool enough to condense into a narrow band of cloud. Depending on wind conditions, the wave may be ‘standing’, with the peak remaining in the same place for hours, or may move off downstream, and new peaks form behind it, but we would still call it ACSL.These physics are beautifully described and illustrated in a free slim volume, AC 00-57 Hazardous Mountain Winds and Their Visual Indicators . This book was published by the FAA to help pilots understand and identify the strong vertical winds that can result from mountain waves. Figure 2 shows a specific type of mountain wave, the ‘trapped lee wave’, that has multiple wave crests. The wave is ‘trapped’ by shear in the upper atmosphere that prevents the wave energy from propagating upwards. Figure 3 shows a number of time-lapse videos of mountain wave clouds that show how the air moves through the clouds while the clouds remain stationary over the landscape.
ACSL clouds may have smooth edges, as in the classic lenticular shape, with a lentil, or lens shaped cross section, or it may look more turbulent or roughed up, but it probably won’t look like altocumulus clouds formed by unstable air, with flat bottoms and cauliflower tops.Figure 3: Rocky Mountain Wave Clouds by D. Durrand
Glider pilots love the updrafts, but this phenomenon can have devastating effects, even beyond possible plane crashes. The Marshall Fire on December 30, 2021, was a direct consequence of a mountain wave windstorm slamming down onto the plains just east of the Front Range that day, killing two people and destroying over 1000 homes. .
Besides the gravity waves that lead to ACSL clouds, mountains can also cause the rare fluctus, or Kelvin-Helmholtz (K-H) clouds. These form in shear layers, which are where the wind speed changes suddenly with height. Generally the increase in speed with height is gradual, but the speed can change quickly downwind of mountain ranges in stable air. The strong shear results in a layer of vorticity or rotational air, which then collects into a regular series of vortexes: this is the Kelvin-Helmholtz instability . If the top of a cloud coincides with the shear layer, the rotating vortices will pull the cloud into a row of waves , as shown in Figure 4. This can happen almost anywhere in the atmosphere, but is more common near mountains or on top of fog or low stratus clouds, often over bodies of water. The K-H instability is pretty common: it’s easy to study in the laboratory, and occurs in the ocean and even in the sun. But having the right moisture layer at the same time is rare. These conditions are fleeting, so fluctus may last only a few seconds. Do photograph if your see it!
Another orographic cloud that occurs in stable atmosphere is the Foehn (pronounced ‘fawn’) cloud wall that accompanies a Foehn wind . As moist air is pushed up in elevation by the terrain, it cools, condenses and releases moisture, as shown in Figure 5. The resultant clouds are visible just over the mountains, as shown in Figure 6. When the air descends the other side, it heats quickly as it is compressed since it has little thermal inertia compared to moister air, and the clouds evaporate leaving clear air on the leeward (downwind) side. Foehn winds are also called ‘Chinook’ winds after a group of Pacific Northwest indigenous people where the term originated. However, the inland Blackfoot people refer to these winds as ‘snow eaters’ since they occur in winter and are warm and dry enough to make snow sublimate .