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A lenticular cloud covers the summit crater of Mayon Volcano, Philippines.. As air travels along the surface of the Earth, obstructions are often encountered, including natural features, such as mountains or hills, and artificial structures, such as buildings and other constructions, which disrupt the flow of air into "eddies", or areas of turbulence.
A pileus (/ ˈ p aɪ l i ə s /; Latin for 'cap'), also called scarf cloud or cap cloud, is a small, horizontal, lenticular cloud appearing above a cumulus or cumulonimbus cloud. Pileus clouds are often short-lived, appearing for typically only a few minutes, [ 1 ] with the main cloud beneath them rising through convection to absorb them.
Lenticular clouds form when strong northwesterly winds flow up and over the mountain range, creating a standing wave. The air cools as it rises, and the water vapour in the air condenses to form clouds. The Taieri Pet cloud formation can sometimes appear in layers and has been described as a "huge stack of plates" in the sky.
The peculiar cigar-shaped cloud is called an altocumulus standing lenticular cloud (ASLC) and is created when winds encounter a steep barrier such as a mountain range, Nasa explained in a statement.
Lenticular Clouds Shrouding the Peaks of Mount McKinley (Getty Images/Ron Sanford) On June 24, 1947, pilot Kenneth Arnold reported seeing multiple mysterious, gleaming circular objects along the ...
If you have seen a cloud that looks like a UFO, it might have been a mesmerizing lenticular cloud. These fascinating formations are caused by waves in the atmosphere. When air blows into a ...
A cap cloud is a special form of the lenticular cloud with a base low enough that it forms around and covers the peak, capping it. [3] A chinook arch cloud is an extensive wave cloud. It has this special name in North America where it is associated with the Chinook wind. It forms above the mountain range, usually at the beginning of a chinook ...
Stratocumulus lenticularis is an uncommon cloud type that belongs to the stratocumulus cloud type, its appearance is that of a flat lens or almond.It forms as a result of atmospheric waves [1] caused by wind passing over obstacles; for example, a mountain or a building.