#circumzenithal arc

[bluecapsicum]

Cold winter skies illustrations for my daily meteorological fiction project, Reports From Unknown Places About Undescribable Events (Twitter, Instagram, Mastodon).

Keep reading for captions.

December 24th - We report: once again, we find ourselves under a murmuration as we walk past a field. We can hear trills and whistles coming from this massive bird cloud waltzing in the winter sky. We think there might be a few hundred of them, all moving together. We stay there for a long time.

January 10th - We report: the sky so dark and low this way, and the horizon so far, the trees bare and tiny in the distance; we wonder whether there might be space enough between the sky and the earth for us to walk. As it is, our face is up in the sky and our feet are down in the frozen earth.

January 13th - We report about this time, late in the afternoon when the humidity starts to saturate the atmosphere. Even through the dense clouds, there are faint hints of sunset colours amidst the grey. Blackbirds and sparrows are getting busy while we wait for the rain.

January 18th - We report Jupiter and Saturn at nightfall today; we expect Venus to follow shortly after, although the sky might be overcast by then. It is still too bright for us to be able to see stars, but we know that the Aquarius constellation is right there, rising over the horizon.

January 21st - We report: a morning removed from the world, fog and frost making even time move sluggishly. Every blade of grass looks brittle, and we wonder if they would snap off immediately, should we touch them. We cannot locate the sun, though we know where it should be.

January 25th - We report: the frothing winter sea during high tides; any colder and it would freeze solid, it would seem. There is an icy blue in the waves that unrelentingly crash against the rocky shore. The day stretches under an opaque sky that remains the same throughout.

January 30th - We report that we lost a glove on this snowy path, and we tried to walk back in our earlier steps. It was easy at first, but the snow and the night kept falling steadily; the footsteps disappeared. When we finally came home, though, our expert told us that they had picked it up.

February 13th - We report a very rare and complex halo display: a 20° halo, a parhelic circle with parhelia, a sun pillar leading up to an upper tangent arc and a parry arc, a 46° halo, and a circumzenithal arc. Very complex indeed, many arcs for a single sun. It is absolutely freezing outside.

February 22nd - We report: in the car, on a parking lot, facing the ocean. The rain is hitting the windscreen hard, in waves. It is an old car; the wind shakes it and whistles through the small cracks where the doors do not close very well. We watch raindrops run down the windows at an angle.

March 14th - We report: it has not stopped being cold here. We walk in the footsteps of someone who was here earlier this morning. It has snowed a little bit again since, and some of the tracks have been filled in. We are following a line of pollarded trees that creak in the cool wind.

[mrvelocipede]

[yuka-p]

今朝5:20過ぎの空。

虹（左）と環天頂アーク（右）が少しだけ見えました。

[apod]

2023 December 20

Ice Halos over Bavaria Image Credit & Copyright: Bastian Werner

Explanation: What's causing those unusual sky arcs? Ice crystals. While crossing a field of fresh snow near Füssen, Bavaria, Germany, earlier this month, the photographer noticed that he had entered an ice fog. For suspended water to freeze into an ice fog requires quite cold temperatures, and indeed the air temperature on this day was measured at well below zero. The ice fog reflected light from the Sun setting behind St. Coleman Church. The result was one of the greatest spectacles the photographer has ever seen. First, the spots in the featured picture are not background stars but suspended ice and snow. Next, two prominent ice halos are visible: the 22-degree halo and the 46-degree halo. Multiple arcs are also visible, including, from top to bottom, antisolar (subsun), circumzenithal, Parry, tangent, and parhelic (horizontal). Finally, the balloon shaped curve connecting the top arc to the Sun is the rarest of all: it is the heliac arc, created by reflection from the sides of hexagonally shaped ice crystals suspended in a horizontal orientation.

∞ Source: apod.nasa.gov/apod/ap231220.html

[just--space]

Ice Halos by Moonlight : An almost full moon on April 15 brought these luminous apparitions to a northern spring night over Alberta Canada. On that night, bright moonlight refracted and reflected by hexagonal ice crystals in high clouds created a complex of halos and arcs more commonly seen by sunlight in daytime skies. While the colors of the arcs and moondogs or paraselenae were just visible to the unaided eye, a blend of exposures ranging from 30 seconds to 1/20 second was used to render this moonlit wide-angle skyscape. The Big Dipper at the top of the frame sits just above a smiling and rainbow-hued circumzenithal arc. With Arcturus left and Regulus toward the right the Moon is centered in its often spotted 22 degree halo. May 15 will also see the bright light of a Full Moon shining in Earth's night skies. Tomorrow's Full Moon will be dimmed for a while though, as it slides through Earth's shadow in a total lunar eclipse. via NASA

[thefirststarr]

SPACEMAS DAY 23 ✨🪐🌎☄️☀️🌕

Since it’s officially winter now (in this hemisphere at least) I thought this picture for today would be fitting!!

What's causing these unusual sky arcs? Ice crystals! While crossing a field of fresh snow near Füssen, Bavaria, Germany, this photographer noticed that he had entered an ice fog. For suspended water to freeze into an ice fog requires quite cold temperatures, and the air temperature on this day was measured at well below zero. The ice fog was reflecting light from the sun setting behind St. Coleman Church. The result was this spectacular image. First, the spots in the featured picture are not background stars but suspended ice and snow. Next, two prominent ice halos are visible: the 22-degree halo and the 46-degree halo. Multiple arcs are also visible, including, from top to bottom, antisolar (subsun), circumzenithal, Parry, tangent, and parhelic (horizontal). Finally, the balloon shaped curve connecting the top arc to the Sun is the rarest of all: it is the heliac arc, created by reflection from the sides of hexagonally shaped ice crystals suspended in a horizontal orientation.

Image Credit & Copyright: Bastian Werner

[mutant-distraction]

A couple of circumzenithal arcs captured at Smuggler’s Notch VT

[fernthewhimsical]

Different types of rainbows

Did you know there are different types of rainbows? Us witches love our correspondences, so in Rainbowmancy we can tap into each of these rainbow energies to charge items or power our magic.

Primary rainbow: Our beloved rainbow. Rain droplets catch sunlight which creates a prismatic effect, causing the arc of colours to appear. In a primary rainbow we see red on the outer edge of the arc, and violet on the inner edge. A rainbow is actually a circle, but we are most often too close to the ground to see it in its entirety. Higher up this "full circle rainbow" as it's called, becomes visible

Double rainbow: This is when a, usually paler, secondary rainbow appears above of our primary rainbow. The second rainbow has their colours reversed, with violet on top and red in the centre.

Twinned rainbows: Here the two rainbows are not stacked, but instead appear to begin at the same base, splitting off from there. Where with the double rainbow the colours are reversed, the twin rainbow has the same order of colours as the primary rainbow.

Monochrome rainbow: A very dramatic looking rainbow in just red. This happens when there is a rain-shower at sunset or sunrise.

Supernumerary rainbows: Also knows as "stacker rainbow" or "supernumerary bands". Here bands of pastel rainbow colours appear just below the inner arc of the primary rainbow. The colours are more pastel, and keep repeating, fading the further away from the arc they go. Rarely supernumerary bands can also be stacked on the top of the primary rainbow.

Reflected rainbow: When the primary rainbow is reflected in a body of water, even as small as a puddle. After deflecting in the raindrops the light reflects off of the water.

Reflection rainbow: Here the light first reflects off of a big body of water before deflecting in the raindrops. Reflections of the primary rainbow can be seen, sometimes up to eight in number!

Fogbow: These rainbows are made when the light is refracted in the tiny droplets of fog or mist. Because of the dispersion they are mostly white, with some reds and blues. The bands of colour are broad, but very muted. They often appear with a Glory in the centre (see below).

Moonbow: Not only the light of the Sun can bring a rainbow, the light of the Moon can as well! This is rare, and requires the moon to be close to full. Our human eyes often see the moonbows as white, for we can't see the colours, but they are there.

Snow rainbow: Also known as a sleet rainbow. These look like primary rainbows, however here the light is refracted through ice pellets instead of liquid raindrops. Sleep rainbows can also have double, twinned, monochrome, and other forms of rainbow. Other optical phenomena that are similar to rainbows, but not actually rainbows:

Circumhorizontal and circumzenithal arcs: This happens when light is refracted in hexagonal ice crystals instead of raindrops. The circumhorizontal arc is more flat than the circumzenithal arc, which looks almost like an upside down rainbow. Both have the red parts of their arc pointed towards the Sun (or Moon).

Glory: This appears around a shadow cast in mist of fog. The reflection in the tiny droplets causing a multicoloured halo to appear around the shadow. The "halo" starts with red and ends with blue, repeating itself and growing less bright with each repeat.

Rainbow spiderwebs: Dew catches on the strand of a spiderweb. The droplets then refract light, creating a glowing rainbow web of colours

Cloud iridescence: An optical phenomenon that occurs when thin clouds close to the Sun or Moon contain water droplets or ice crystals that are roughly the same size. The light is refracted within the cloud which creates repeating bands of colour.

Iridescence: Also known as goniochromism. Iridescence means "having a tendency towards rainbows", meaning that although they are not truly rainbows, their colouring does remind us of it. It is an optical phenomenon where the colours shift depending on in which angle the light hits it. Very thin layers of the surface then refract light back in different wavelengths, making it appear to shift colour and have multiple colours. Examples are soap bubbles, oil slick, feathers, butterfly wings, and certain crystals, such as opals.

Pearlescence: The same phenomena as iridescence, but most of the light reflected back is white.

[Part of a Rainbowmancy series, masterpost here]

[iwillruletheuniverse]

The sky gave a circumzenithal arc today🫶🏻 Felt very special to see🩵

[mx-metronome]

Small parhelion to the left of the sun, circumzenith arc above my head

[galswintha]

Partly developed circumscribed halo with circumzenithal arc.

[robinsonprojection]

Here is a Halo Display I took some pictures of the day before the big storm on Christmas, the extreme cold and high wind speed picked up a large amount of snow and ice, which refracted the sunlight according to the structure of the ice, resulting in several common halos and one weird one.

Pictures below show the annotated image and a guide to Halos I put together last year.

In this display are the following:

Sun Dogs (Parhelia) - The most common halo component, formed as sunlight is refracted through plate shaped hexagonal ice crystals gently floating downwards.

22° Halo - Another common halo, forms as light is refracted through hexagonal plates in a state besides being completely flat, resulting in a ring around the sun at the same distance as the sun dogs.

Parhelic Arc - A less common halo caused by reflection off of the surface of ice crystals rather than refraction. This particular instance only stretched through the sun rather than all the way around the sky, which is common when it appears at all.

Bravais Arc (Circumzenithal Arc) - A reasonably common halo that has a reputation for being rare since it is seen at such a high altitude compared to others. This halo forms a rainbow arc in a circle around the zenith when the sun is at most 30° above the horizon. Caused by light entering the top of a hexagonal ice crystal and exiting through its side, resulting in a separation of colors.

[explosiveforce]

Clouds are amazing, and there’s an official Cloud Spotters Club you can join!

On another note, THE FIRST PHOTO HAS A CIRCUMZENITHAL ARC. This is a rare lighting affect where light bounces off small ice crystals in the upper atmosphere (mostly in cirrus clouds). The end result is a rainbow smile.

If anyone is interested in learning more about clouds, I HIGHLY recommend The Cloud Spotter’s Guide by Gavin Pretoria-Pinney.

People are like “it’s so beautiful no clouds at all” it could use a little clouds if I had to be honest.

[yuka-p]

薄っすらと環天頂アークとハロ。

[nakashima-antenna]

impressesky III – DualSide

空の情景をイメージした Liquid Funk アルバム Tr.04「Circumzenithal Arc」

■BOOTH ■bandcamp

[just--space]

When Rainbows Smile : Want to see a rainbow smile? Look near the zenith (straight up) when the sun is low in the sky and you might. This example of an ice halo known as a circumzenithal arc was captured above a palm tree top from Ragusa, Sicily on February 24. The vividly colorful arcs are often called smiling rainbows because of their upside down curvature and colors. For circumzenithal arcs the zenith is at the center and red is on the outside, compared to rainbows whose arcs bend toward the horizon after a downpour. True rainbows are formed by water droplets refracting the sunlight to produce a spectrum of colors, though. Circumzenithal arcs are the product of refraction and reflection in flat hexagonal ice crystals, like the ice crystals that create sundogs, formed in high thin clouds. via NASA