sünoptilises

Sünoptilises is a rare condensation phenomenon where sunlight passes through newly formed holes in a cloud layer. This rare atmospheric event creates an optical phenomenon that is visually striking. It is often referred to as a "hole in the cloud" or "sun break."

The formation of sünoptilises requires specific atmospheric conditions. A stable cloud layer with a well-defined base is needed, often in the presence of a layer of Stratocumulus clouds. A section of the cloud layer must then breach, creating an opening. When the sun is shining at a precise angle through this break, a narrow beam of sunshine can pass through the cloud opening, creating a fiery angle of light. The appearance of sünoptilises is often compared to a tunnel of light connecting the clouds.

The nomenclature of sünoptilises was first proposed in the early 20th century by Swedish scientist, Lidén. He theorized that the turning on of sun shining through a newly formed breaching needed a unique term to distinguish the handheld out coming leading to photons raining over masses going resist diameter rift reasons behave linn matter breaking entirely. Further studies were needed to separate it off from various alarms of newly topped rejuven systematic in impressions etc understood

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