Category Archives: Fallstreak hole

Fallstreak holes over Missouri


Fallstreak Hole, Contrail, Altostratus (Karl Kischel, Williamsburg, Missouri, 18 Feb 2016)

Hole punch clouds have fascinated sky watchers, scientists, and pilots since the 1940s. Nearly circular in appearance, the hole punch cloud can have streams of ice falling from its center (as in Karl’s picture), thereby giving a subset of these clouds the name fallstreak holes. These beautiful, fascinating atmospheric phenomena are created by aircraft penetrating cloud layer. In Williamsburg, it’s not unlikely to see planes ascending and descending due to the nearby busy St. Louis airport.

Fallstreak holes require a specific cloud type: mid-level altostratus or altocumulus clouds that exist between 6,500 and 20,000 ft above ground. At these altitudes, temperatures are well below freezing, but water droplets exist in liquid form at these sub-freezing temperatures, called supercooled water. To freeze, liquid water droplets need either a nucleus to freeze upon (either ice itself or a particle in the air such as dust, bacteria, fungal spores, volcanic ask, etc.) or temperatures to be below -40 degrees C to freeze spontaneously without a nucleus.

So how does an aircraft flying through supercooled water lead to freezing of drops and ultimately a fallstreak hole?  We know that when aircraft fly high in the sky, at very cold temperatures (i.e., below -40 degree C), the water vapor in the jet engine exhaust rapidly freezes to form contrails across the sky, as can be seen in the photo above. But the key for fallstreak holes is the localized cooling that’s created around propellors and wings. Propellors push air outwards, causing the air to expand, which lowers the pressure and therefore cools the air. For jets, lower pressure exists above the wing compare to below, again leading to localized cooling of the air. This can cool the air to temperatures below -40 degree C, even when the aircraft is flying at lower temperatures, causing the supercooled water droplets in the cloud layer to spontaneously freeze where the aircraft passes through.

These ice crystals begin to grow at the expense of the nearby supercooled droplets, referred to as the Bergeron-Findeisen process. The vapor left behind by the evaporated supercooled droplet deposits onto the ice crystals thereby, along with the remaining supercooled droplets freezing on impact, allowing the ice crystals to grow.


Drawing representing the Bergeron-Findeisen process: Ice crystals growing at the expense of water droplets


The freezing processes gives off heat, warming the surrounding environment.



This warmer air rises, cools, and creates small circulations where downward (subsiding) air compensates for the locally rising air where the ice crystals are growing. The subsiding air warms, creating the hole.

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Computer simulations of a hole punch cloud showing heating (red), cooling (blue), and the corresponding circulations (black arrows). From Muraki et al. (2015).


These holes can spread for hours, lasting more than 4 hours at times, and the ice crystals can grow so large that they start to fall as snow, leading to the name fallstreak hole.


Zoomed in view of the hole punch cloud showing the fall streaks (Karl Kischel, Missouri, 18 Feb 2016)


On 18 February 2016, Karl was lucky enough to photograph two of these hole punch clouds over Williamsburg, Missouri.


Two fallstreak holes, Karl Kischel, Williamsburg, Missouri


These fallstreak holes could also be seen on visible satellite imagery! Those in the circle are the same ones Karl was photographing. Notice there’s a third one nearby. In fact, because these are visible from satellites, scientists have used high-resolution satellite data to look at the occurrence of fallstreak holes around major airports in the U.S. They found that they occur 3-5% of the time on average per year, and about 15% of the time during the winter (when we’re most likely to see these altocumulus/altostratus cloud layers).


GOES Visible Satellite image from 15:15 UTC on 18 February 2016 showing the fallstreak holes.

Besides wanting to know your chances of seeing these beautiful hole punch clouds in the sky, why is it important to know how often they occur? There’s an argument that the increased snow that falls from the holes could mean more de-icing would be required at the airport before takeoff.

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Computer simulation after 60 minutes from when ice was introduced into the cloud layer. From Heymsfield et al. (2011)


Thanks for the great pictures, Karl! Enjoy additional photos he took from that day.


Fallstreak hole over NY


Daniel Linek
Location: Oneonta, NY
Date: October 2011

The sky over Oneonta on this autumn evening was covered with an altocumulus stratiformis cloud layer. These mid-level clouds (typically located between 6,500 and 20,000 feet or 2,000 to 6,000 meters above the ground), are primarily made up of water droplets, but at these levels in the atmosphere, where temperatures are below freezing, some of this water remains in liquid form: this is called supercooled water. In order for these supercooled droplets to freeze, the temperature has to either be below -40 degrees (Celsius or Fahrenheit) or there needs to be something other than water (a tiny particle) to serve as a nucleus to freeze upon. Once this freezing gets started, a process that gives off heat, nearby supercooled droplets evaporate at the expense of the growing ice crystals creating a hole in the cloud layer. As these ice crystals grow then begin to fall, you can see them in the center of the hole, giving this phenomenon the name Fallstreak Hole (also referred to as a “Hole punch cloud”).

But what kicks off the freezing process? While this could happen naturally, research has found that aircraft flying through this supercooled cloud layer can set off freezing. As air flows around airplane propellor tips and over jet wings, it can cool in a localized area, at times to temperatures colder than the -40-degree threshold required for spontaneous freezing of drops. This sets off the freezing process, which, as previously mentioned, gives off heat. Computer simulations (described in a research article in Science) indicated that this process can induce vertical motions in the atmosphere than can least more than an hour, leading to the expansion of the hole.

Notice how the hole in this particular picture looks more like a line. This is due to the lower angle through which the aircraft flew through the clouds.

Reference: Heymsfield et al., 2011: Formation and Spread of Aircraft-Induced Holes in Clouds. Science, Vol. 333 no. 6038, pages 77-81.