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Saturday, January 31, 2015

Holes in the clouds - hole punch or fallstreak hole clouds.

We were in South Carolina today & saw a hole in the clouds over the town of Lancaster. It was such a rare sight & strange feeling to watch this. We took a few pictures before it disappeared.







My research revealed per the Weather Channel:

These rare cloud formations, called "hole-punch clouds", develop in altocumulus cloud layers and are often the result of airplanes passing through the layer of clouds.
So, how does this happen?
The altocumulus cloud layer is composed of small water droplets that are below freezing called supercooled water droplets. If ice crystals can form in the layer of supercooled droplets, they will grow rapidly and shrink or possibly evaporate the droplets completely.

and National Geographic:


Clouds are made of water droplets, and hole punch clouds—also known as fallstreak hole clouds—occur when part of that cloud falls out, leaving behind a hole. That opening in the cloud is the result of an extremely localized snowfall.
Usually, atmospheric water droplets latch on to particles in order to form ice crystals, or snow. This happens on a massive scale during snowstorms. The only way water droplets can spontaneously form ice crystals without those particles is if temperatures fall to roughly -40°F (-40°C). (Learn more about these giant cloud holes.)
In a hole punch cloud, temperatures fall in only a small portion of the cloud, forming a localized snowstorm. When that snow falls, it leaves behind a hole. Refraction of sunlight by the ice crystals results in the rainbow, while the arrangement of those crystals gives us a bright patch of light in the middle called a sun dog. (See pictures of sun dogs and halos.)
The expansion of air as an airplane passes can also produce hole punch clouds by cooling water droplets enough for them to form ice crystals.

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