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That wave cloud pattern formed over the Île Amsterdam, in the lower left corner at the tip of the triangular formation, in the far southern Indian Ocean. A wave cloud is a cloud form created by atmospheric internal waves. Wave cloud pattern in Tadrart region. Unusual wave clouds over the Aral Sea, seen from NASA's Water satellite on March 12 ...
The island generates wave motion in the wind passing over it, creating regularly spaced orographic clouds. The wave crests raise and cool the air to form clouds, while the troughs remain too low for cloud formation. Note that while the wave motion is generated by orographic lift, it is not required. In other words, one cloud often forms at the ...
1671 – Anglo-Spanish War: In pursuit of retreating Spanish troops, English soldiers sacked the city of Panama. 1916 – The province of Manitoba passed a law that first granted some Canadian women the right to vote. 1941 – About three hours after Thai bombers raided Sisophon, a ceasefire paused hostilities in the Franco-Thai War.
"Tail": A tail cloud that extends horizontally away from the murus cloud and is the result of air feeding into the storm. Cumulonimbus murus cauda Fluctus Crested wave-like stratocumulus, altocumulus, or cirrus cloud formed by wind-shear. Stratocumulus fluctus Incus "Anvil": Top part of a mature cumulonimbus cloud; anvil-shaped feature.
The altostratus undulatus is a type of altostratus cloud with signature undulations within it. These undulations may be visible (usually as "wavy bases"), but frequently they are indiscernible to the naked eye.
This is an accepted version of this page This is the latest accepted revision, reviewed on 22 January 2025. Visible mass of liquid droplets or frozen crystals suspended in the atmosphere "Nephology" redirects here. Not to be confused with Nephrology. For other uses, see Cloud (disambiguation). Cloudscape over Borneo, taken by the International Space Station Part of a series on Weather ...
Orographic fohn cloud over La Palma, Canary Islands Wave clouds Lenticular clouds with rotor clouds underneath. A Föhn cloud or Foehn cloud is any cloud associated with a Föhn (Foehn), usually an orographic cloud, a mountain wave cloud, or a lenticular cloud. Föhn is a regional term referring to winds in the Alps.
Waves may also form in dry air without cloud markers. [4] Wave clouds do not move downwind as clouds usually do, but remain fixed in position relative to the obstruction that forms them. Around the crest of the wave, adiabatic expansion cooling can form a cloud in shape of a lens (lenticularis). Multiple lenticular clouds can be stacked on top ...