'Atmospheric Phenomene' images and/or videos results page 1 of 2

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter

Sebastien Beaucourt

PIX4671067

Rainbow Rainbow Panoramic of 6 Vertically Assembled Photos

Patrick Lécureuil

PIX4671222

Green ray - Green flash - Green ray obtained during sunset. Green flash during a sunset

Guillaume Blanchard

PIX4629143

Blue ray - Blue flash - Blue ray obtained during sunset. Blue flash during a sunset

Sebastian Voltmer

PIX4629255

Arc de fog - Fogbow - Arc de brume observed in Brittany on February 23, 2008. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on Feb 23, 2008. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted

Laurent Laveder

PIX4671411

Mother-of-pearl cloud - Nacreous clouds - Mother-of-pearl cloud observed in Lapland. Nacreous cloud (or polar stratospheric cloud) seen in Lapland, Finland

Sauli Koski

PIX4671586

Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671433

Sebastien Beaucourt

PIX4671044

Rainbow - Rainbow - Detail of a rainbow with supernumerary arches. Detail of a rainbow with supernumerary rainbow. July 11, 2008

Laurent Laveder

PIX4671124

Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009

Laurent Laveder

PIX4671301

Alex Tudorica

PIX4671058

Sunset - Sunset: The solar disk, behind a layer of Earth's atmosphere, deforms a lot - The Sun distorted by Earth's atmosphere layer

Sebastian Voltmer

PIX4629000

Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009

Laurent Laveder

PIX4671332

Double rainbow (photo)

Patrick Lécureuil

PIX6039659

Sunset and Blue Ray - Sunset - Blue flash - Blue ray obtained during sunset in Hawaii. October 2004. Blue flash during a sunset in Hawaii. October 2004

Martin Rietze

PIX4629152

Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009

Laurent Laveder

PIX4671314

Iridescent cloud - Iridescent cloud - Iridescent and solar crowns in clouds caused by water drops of similar diameter. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds

Laurent Laveder

PIX4671552

Anticrepuscular rays - Anticrepuscular rays - Crepuscular rays opposite the sun. Chile. Crepuscular rays seen opposite the sun in the sky. Chile

Alex Tudorica

PIX4672203

Corona around the Moon - Corona around the Moon - When the light of the Moon passes through thin clouds of water droplets, it can create a moon crown of color. In meteorology, a corona is produced by the diffraction of light from the Moon by small water droplets in a cloud

G. Cannat

PIX4671760

Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

Sebastian Voltmer

PIX4671365

Sunset - Sunset - Sequence of a sunset deforms by layers of thermal inversion in the atmosphere. Different views of a sun setting distorted by multiple temperature inversion layers

Guillaume Blanchard

PIX4628767

Sunset - Sunset - Sequence of a sunset deforms by layers of thermal inversion in the atmosphere. Different views of a sun setting distorted by multiple temperature inversion layers

Guillaume Blanchard

PIX4628773

Halo around the Moon - Lunar halo - This halo is due to the light of the full moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Moon. Image obtained on February 8, 2009. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo that is 44 degrees in diameter. February 8 2009

Laurent Laveder

PIX4671714

Green ray - Green flash - Green ray obtained during sunset. Green flash during a sunset

Guillaume Blanchard

PIX4629148

Sebastien Beaucourt

PIX4671056

Rainbow Rainbow Rainbow Rainbow July 11, 2008 Rainbow July 11, 2008

Laurent Laveder

PIX4671119

Solar Parhely - Sun dog - Parhelies are the optical phenomena caused by the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

Patrick Lécureuil

PIX4671383

Laurent Laveder

PIX4671753

Sunset and inferior mirage - Sunset and inferior mirag

Guillaume Blanchard

PIX4628749

Sunset and inferior mirage - Sunset and inferior mirag

Guillaume Blanchard

PIX4628782

Paraselene on a full moon night - Moon dog - A paraselene consists of light spots located on the left and right at the height of the Moon; they are equivalent to the parhelies of the Sun. These glowing patch is named Moon dog. Moon dogs are the same phenomenon as the sun dogs for the Sun

Patrick Lécureuil

PIX4671658

Parhely - Sun dog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. The parhely is clearly off the halo of 22* radius when the Sun is 21* high. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

Laurent Laveder

PIX4671367

Alex Tudorica

PIX4671060

Sunset and inferior mirage - Sunset and inferior mirag

Guillaume Blanchard

PIX4628743

Iridescent clouds - Iridescent clouds - When parts of a cloud are very thin and contain water droplets of the same size, the diffraction of the solar light that passes through them can cause colour comparable to those of crowns. We are talking about iridescent or iridescent clouds. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds

G. Cannat

PIX4671608

Rainbow on the Great Ocean Road - Rainbow seen while driving on the Great Ocean Road, Victoria, Australia on Jun 11, 2011

Jia Hao

PIX4671257

G. Cannat

PIX4671618

Colored crown around the Sun - Corona around the Sun - Crown or dark circles are light phenomena produced by the diffraction of light by droplets in the clouds. In meteorology, a corona is produced by the diffraction of light from the Sun by small water droplets in a cloud

G. Cannat

PIX4671797

G. Cannat

PIX4671001

G. Cannat

PIX4671604

G. Cannat

PIX4671615

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. February 2010. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. February 2010

Patrick Lécureuil

PIX4671043

Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008

Laurent Laveder

PIX4671130

Arc - en - lunar sky - Lunar Rainbow - Arc - en - lunar sky causes not by the light of the Sun, but by that of the Moon. 10/02/2009 Rainbow made by moonlight. February 10 2009

Laurent Laveder

PIX4671291

Green ray - Green flash during a sunset - Green ray obtained during a sunset. Green flash during a sunset

Guillaume Blanchard

PIX4629123

Sunset on a church - 1/3 - Sunset above a church - 1/3 - Sunset on the church of Agia Eleousa in Greece. 25 November 2009. The foreground is the Church of Agia Eleousa which lies atop a mountain at an altitude of approximately 165 meters (500 feet), northeast of Athens. The photo was taken from a distance of 3495 meters away to the east of Agia Eleousa so as to yield a reasonable balance in the aspect ratio involving the foreground church and setting sun as well as to provide the ideal azimuth and altitude for these photos to be possible. November 25, 2009

PIX4628856

Laurent Laveder

PIX4671707

Halo around the Moon - Lunar Halo - Halo around the Moon observes a few hours before the full Moon on January 10, 2009. The paper pencil-shaped ice crystals present in the cirrus form the lunar light (in fact, the solar light reflected by the lunar surface) as small prisms and can give birth to this large coloured circle (red inside and blue outside). Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo that is 44 degrees in diameter. January 10 2009

G. Cannat

PIX4671727

Lunar Halo - Lunar Halo - Lunar Halo. The ice crystals in the cirrus decompose the lunar light (in fact, the solar light reflected by the lunar surface) as small prisms and can give rise to a large coloured circle. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo that is 44 degrees in diameter

Patrick Lécureuil

PIX4671730

Parhelia - Sundog - Parhelies are optical phenomena due to the interaction of solar light on ice crystals. Sundogs appear generally when the sun is low, and the atmosphere is filled with ice crystals forming cirrus clouds; they are caused by the refraction of sunlight passing through ice crystals

Alex Tudorica

PIX4671368

Laurent Laveder

PIX4671560

Solar column - Solar pillar - A solar column is created by the reflection of solar light on the horizontal faces of ice crystals. It therefore requires a fairly stable atmosphere to keep these crystals parallel to the horizon. 16 June 2006, Finistere. A solar pillar is created by the reflection a sunlight (when sun is at or low to the horizon) on the horizontal face of ice cristals. So, a quiet atmosphere is needed in order that this cristals stay parallel to the horizon. June 16 2006, Brittany, France

Laurent Laveder

PIX4671473

G. Cannat

PIX4671609

Halo around the Moon - Lunar Halo - This halo is due to the light of the Moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and thus create a perfect circle around the Moon. 29 November 2007. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. November 29, 2007

Laurent Laveder

PIX4671705

Pearl clouds, Norway, 2020 (photo)

Alex Conu

PIX6039662

Guillaume Blanchard

PIX4671025

Lower Mirage - Inferior mirage - Lower Mirage on Lake Titicaca. The difference in temperature between water and air gives the illusion that the Earth is reflecting itself, coupled with a reverse image. Inferior mirage on the lake Titicaca. Inferior mirages are caused by the differences of temperature between sea and air which produce an inverted image below

Guillaume Blanchard

PIX4672048

Corona around the Moon - Corona around the Moon - When the light of the Moon passes through thin clouds of water droplets, it can create a moon crown of color. In meteorology, a lunar corona is produced by the diffraction of light from the Moon by small water droplets in a cloud

K.A Lecky Hepburn

PIX4671781

Guillaume Blanchard

PIX4671029

K.A Lecky Hepburn

PIX4671763

Moon and Jupiter - Moon and Jupiter - Planet Jupiter (the bright spot on the left) near the Moon. Image obtained on July 17, 2008. To the left of nearly full moon is the bright planet Jupiter. Image taken on July 17, 2008

Laurent Laveder

PIX4587513

Paraselene - Moon dog - A paraselene consists of light spots located on the left and right at the height of the Moon; they are equivalent to the parhelies of the Sun. On the left of the Moon, the bright spot is the planet Jupiter. Image obtained on July 17, 2008. These glowing patches on the right and left at the Moon's elevation are named Moon dog. Moon dogs are the same phenomenon as the sun dogs for the Sun. To the left of nearly full moon is the bright planet Jupiter. Image taken on July 17, 2008

Laurent Laveder

PIX4671663

Rainbow Rainbow Rainbow with Alexander's Band, a darker region of the sky above the primary arc and below the secondary arc. 10 December 2007. Rainbow with Alexander Dark Band, a darker area between the primary and the secondary rainbow. December 10 2007

Laurent Laveder

PIX4671105

Pearl clouds in Oslo, Norway, 2020 (photo)

Alex Conu

PIX6039510

Conjunction Venus Jupiter - Jupiter-Venus conjunction - Venus (the brightest) and Jupiter seen above the horizon. Each planet presents a short light column. Riviere Odet, Brittany. 24/11/2008 Venus (the brightest) with Jupiter seen above the horizon. Both planets have a short pillar. Odet river, Brittany. November 24, 2008

Laurent Laveder

PIX4587473

Pearl clouds, Norway, 2020 (photo)

Alex Conu

PIX6039661

Venus belt - Earth's shadow - Panorama obtained shortly after sunset showing the shadow of the Earth projected on the sky. This blue - grey area is called an anti-repuscular arch or Venus belt. November 1, 2007. Panorama showing Earth's shadow projected onto the sky. It is visible as a blue - gray zone. This phenomena is called the belt of Venus

Laurent Laveder

PIX4672115

Laurent Laveder

PIX4671499

Observation of pearly clouds, Norway, 2020 (photo)

Alex Conu

PIX6039664

Sebastian Voltmer

PIX4671779

Observation of pearly clouds, Norway, 2020 (photo)

Alex Conu

PIX6039663

Boyden Observatory - South Africa - Boyden observatory - South Africa - Rainbow above the cupola of the 1.5 metre telescope. Bloemfontein, South Africa. Rainbow and the 1.5 m telescope dome. Bloemfontein, Republic of South Africa

Guillaume Blanchard

PIX4651767

Venus Belt - Earth's shadow - The Castle of Assas (Herault), in front of the dark blue bar of the anti-repuscular arch, topped by the pink glow of the Venus Belt. 23 December 2008. Image showing Earth's shadow projected onto the sky. It is visible as a blue - gray zone. This phenomena is called the belt of Venus. Castle of Assas, Herault, France. December 23 2008

G. Cannat

PIX4672145

Full Moon rise in summer - Full Moon rise in summer - The heat mist that borders the horizon at the end of the summer day contributes to make the moon rise particularly spectacular by blushing its face. At the ground level, the turbulence of the atmosphere flattenes and becomes the lunar globe. July 2005. Full Moon is rising with a reddish face due to warm atmosphere. July 200

G. Cannat

PIX4578961

Guillaume Blanchard

PIX4651780

Guillaume Blanchard

PIX4651772

Rainbow in Lapland - Rainbow in Lapland - Rainbow in Lapland, region of enontekioe (Finland), August 2005. Rainbow above Lapland landscape, enontekioe kilpisjarvi, Finland. August 2005

Sauli Koski

PIX4671161

Colored crown around the Moon and irizations - Corona around the Moon with irisation - Provoked by the microscopic drops of water that form these clouds, the crowns are colored blue as close to the Moon, then degrade from yellow to brick red. In the distance, on the edge of the cloud strip, another luminous phenomene is noticeable: these are colourful irisations such as those seen sometimes on some puddles. In meteorology, a lunar corona is produced by the diffraction of light from the Moon by small water droplets in a cloud

G. Cannat

PIX4671856

Nacreous clouds - Nacreous clouds - PSC for Polar Stratospheric Cloud observed in Norway. Nacreous cloud (or PSC for polar stratospheric cloud) seen in Norway

Alex Conu

PIX4634029

Nacreous clouds - Nacreous clouds - PSC for Polar Stratospheric Cloud observed in Norway. Nacreous cloud (or PSC for polar stratospheric cloud) seen in Norway

Alex Conu

PIX4634016

Nacreous clouds - Nacreous clouds - PSC for Polar Stratospheric Cloud observed in Norway. Nacreous cloud (or PSC for polar stratospheric cloud) seen in Norway

Alex Conu

PIX4634036

Rainbow - Rainbow - Rainbow - Sky observed in Brittany in April 2013

Laurent Laveder

PIX4671304

Sea of clouds with shadow of Pic du Midi - The shadow of Pic du Midi projects on the sea of clouds. In the sky there are some anti-crepuscular rays. Shadow of Pic du Midi with anticrepuscular rays

Patrick Lécureuil

PIX4671956

Solar column - Solar pillar - A solar column is created by the reflection of solar light on the horizontal faces of ice crystals. Therefore, a fairly stable atmosphere is needed to keep these crystals parallel on the horizon. 6 February 2006. A solar pillar is created by the reflection a sunlight (when sun is at or low to the horizon) on the horizontal face of ice cristals. So, a quiet atmosphere is needed in order that this cristals stay parallel to the horizon. February 6, 2006, Brittany

Laurent Laveder

PIX4671501

Titan's south pole - Illustration - At Titan's south pole - Artist's view of Titan's surface near the south pole. Artwork

Miller, Ron (b.1947)

PIX4626050

Rainbow Rainbow Double Rainbow Double Rainbow

Sebastien Beaucourt

PIX4671254

Astronaut and Geyser on Enceladus - Artist view - Astronaut and Water geyser on Enceladus - Artist view: An astronaut contemplates the eruption of an ice geyser accompanied by a parhely on the surface of the Enceladus satellite

Miller, Ron (b.1947)

PIX4625922

Rainbow - Rainbow - Double rainbow - Norway. Double rainbow in Norway. Regenbogen - Norwegen - 08/200

Sebastian Voltmer

PIX4671193

Anti-crepuscular rays - Anti-crepuscular rays taken from the Pic du Midi

Patrick Lécureuil

PIX4672247

Torvosaurus and rainbow - A Torvosaurus (Theropode Megalosauridae) walks through the ferns in what is now Colorado 150 million years ago. Weighing nearly two tons, Torvosaurus was one of the largest carnivores of his time. In the sky of the pterosaurs. A Megalosaurid theropod dinosaur of the genus Torvosaurus relaxes among cycads and ferns 150 million years ago in what is today Colorado. In the background are juniper and ginkgo and in the sky flying reptiles of order Pterosauria. A meat-eater that grew to 35 feet long and weighed two tons, Torvosaurus was one of the largest carnivores of its time

Walter B Myers

PIX4662694

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