There were some other worldly looking clouds hovering over the Three Sisters mountains this morning. I took this iPhone photo minutes after the sun illuminated them.
How Lenticular Clouds Form
The Cascade Mountains create a perfect environment for lenticular clouds; we see them quite often. Here’s how they form, courtesy of the National Weather Service’s Albuquerque office.
“Known as Altocumulus Standing Lenticular (ACSL) or Altocumulus Standing Lenticularis clouds, they are associated with waves in the atmosphere that develop when relatively stable, fast moving air is forced up and over a topographic barrier that is oriented more or less perpendicular to the direction from which the upper-level wind is blowing. This deflection creates a gravity wave downwind of the topographic barrier not unlike a wave you might generate by throwing a pebble into a pond. When sufficient moisture is present above mountain-top level, ACSL clouds develop within the crest of these mountain waves where the air is rising. ACSL clouds are continually developing and dissipating in the vicinity of the wave’s crest and immediately downwind of the crest, respectively. That is why they appear to remain stationary (hence the name) even though winds are swiftly (sometimes very swiftly) moving through the entire cloud. They are most often seen in the winter or spring when winds aloft are typically the strongest.”
Lenticular Cloud Eye Candy
As beautiful as these clouds are, a Google image search shows some even more mind-blowing photos of lenticular clouds around the world.
The images will show why they’re called lenticular clouds – many look like lenses. Enjoy!