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'Atmospheric Phenomene' images and/or videos results

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Images of 'Atmospheric Phenomene' found, 142

 
Rainbow over the hills of Lomagne - Rainbow - Rainbow over the hills of Lomagne, Gers, France. Rainbow seen above Lomagne hills, Gers, France

Patrick Lécureuil

PIX4671217

Rainbow over the hills of Lomagne - Rainbow - Rainbow over the hills of Lomagne, Gers, France. Rainbow seen above Lomagne hills, Gers, France

Patrick Lécureuil

PIX4671217

 
Halo and Light Column- Ice halos near Zeel am See, Austria - A light column is created by the reflection of a light source on the horizontal faces of ice crystals. So it takes a fairly stable atmosphere to keep these crystals parallel to the horizon. 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. A paraselene consists of light spots located on the left and right at the height of the Moon. Austria, January 2016. A light pillar is created by the reflection of light on the horizontal face of ice cristals. So, a quiet atmosphere is needed in order that this cristals stay parallel to the horizon. 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

Alex Tudorica

PIX4671758

Halo and Light Column- Ice halos near Zeel am See, Austria - A light column is created by the reflection of a light source on the horizontal faces of ice crystals. So it takes a fairly stable atmosphere to keep these crystals parallel to the horizon. 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. A paraselene consists of light spots located on the left and right at the height of the Moon. Austria, January 2016. A light pillar is created by the reflection of light on the horizontal face of ice cristals. So, a quiet atmosphere is needed in order that this cristals stay parallel to the horizon. 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

Alex Tudorica

PIX4671758

 
Paranal Observatory, Chile - Paranal Observatory, Chile - Yepun, one of the four 8.2m telescopes of the VLT (Very Large Telescope), and two of the four 1.8m auxiliary telescopes. On the horizon, the shadow of the Earth projected on the atmosphere, the belt of Venus (or anticrepuscular arch). January 2008. Paranal Observatory is an astronomical observatory located on the top of Cerro Paranal in the Atacama Desert in the northern part of Chile. This picture shows at left Yepun, one of the four 8,2m telescopes of the Very Large Telescope (VLT), with two auxiliary telescopes. Visible too, the anticrepuscular arch (or belt of Venus, the shadow of earth projected in the atmosphere) January 2008

Guillaume Blanchard

PIX4657124

Paranal Observatory, Chile - Paranal Observatory, Chile - Yepun, one of the four 8.2m telescopes of the VLT (Very Large Telescope), and two of the four 1.8m auxiliary telescopes. On the horizon, the shadow of the Earth projected on the atmosphere, the belt of Venus (or anticrepuscular arch). January 2008. Paranal Observatory is an astronomical observatory located on the top of Cerro Paranal in the Atacama Desert in the northern part of Chile. This picture shows at left Yepun, one of the four 8,2m telescopes of the Very Large Telescope (VLT), with two auxiliary telescopes. Visible too, the anticrepuscular arch (or belt of Venus, the shadow of earth projected in the atmosphere) January 2008

Guillaume Blanchard

PIX4657124

 
Moon rainbow in Norway - Lunar Rainbow in Norway

Alex Conu

PIX4634009

Moon rainbow in Norway - Lunar Rainbow in Norway

Alex Conu

PIX4634009

 
Full Moon - Sardinia - Full Moon - Sardinia

Sebastian Voltmer

PIX4614625

Full Moon - Sardinia - Full Moon - Sardinia

Sebastian Voltmer

PIX4614625

 
Fog bow on the telescope Grantecan - Fogbow above Grantecan - Fog bow above the telescope Grantecan (Gran Telescopio Canarias) 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, 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). Fogbow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary islands

Alex Tudorica

PIX4654492

Fog bow on the telescope Grantecan - Fogbow above Grantecan - Fog bow above the telescope Grantecan (Gran Telescopio Canarias) 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, 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). Fogbow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary islands

Alex Tudorica

PIX4654492

 
Noctulescent clouds, Venus et Mars - Noctilucent clouds, Venus and Mars - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on June 24, 2009 in Ploumanac'h (Cotes d'Armor). On the right, between the two houses, Venus and Mars planets. These high altitude clouds are usually seen in summer months but nearer the poles than France. At right, between the two houses, planets Venus and Mars. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

Laurent Laveder

PIX4587774

Noctulescent clouds, Venus et Mars - Noctilucent clouds, Venus and Mars - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on June 24, 2009 in Ploumanac'h (Cotes d'Armor). On the right, between the two houses, Venus and Mars planets. These high altitude clouds are usually seen in summer months but nearer the poles than France. At right, between the two houses, planets Venus and Mars. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

Laurent Laveder

PIX4587774

 
Anti-crepuscular arch at Pic du Midi - Earth's shadow from Pic du Midi observatory - Photo obtained shortly before sunrise showing the shadow of the Earth projected on the sky. This blue - grey area rose hemmed is called an anti-repuscular arch or Venus belt. Image obtained from the observatory of the Pic du Midi in January 2010. 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. January 2010

Patrick Lécureuil

PIX4655639

Anti-crepuscular arch at Pic du Midi - Earth's shadow from Pic du Midi observatory - Photo obtained shortly before sunrise showing the shadow of the Earth projected on the sky. This blue - grey area rose hemmed is called an anti-repuscular arch or Venus belt. Image obtained from the observatory of the Pic du Midi in January 2010. 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. January 2010

Patrick Lécureuil

PIX4655639

 
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. 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

Alex Conu

PIX4634038

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. 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

Alex Conu

PIX4634038

 
Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

Alex Tudorica

PIX4671634

Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

Alex Tudorica

PIX4671634

 
Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

Alex Tudorica

PIX4671636

Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

Alex Tudorica

PIX4671636

 
Las Campanas Observatory - Magellan Telescope - Las Campanas Observatory - Las Campanas Observatory with Magellan telescopes of 6.5 meters in the foreground on the right. The shadow of the Earth is projected on the sky over the mountains. This blue - grey area rose hemmed is called an anti-repuscular arch or Venus belt. Las Campanas Observatory with the 6.5 meter Magellan twin telescopes in foreground at right. Earth's shadow is projected onto the sky. It is visible as a blue - gray zone. This phenomena is called the belt of Venus

Alex Tudorica

PIX4654264

Las Campanas Observatory - Magellan Telescope - Las Campanas Observatory - Las Campanas Observatory with Magellan telescopes of 6.5 meters in the foreground on the right. The shadow of the Earth is projected on the sky over the mountains. This blue - grey area rose hemmed is called an anti-repuscular arch or Venus belt. Las Campanas Observatory with the 6.5 meter Magellan twin telescopes in foreground at right. Earth's shadow is projected onto the sky. It is visible as a blue - gray zone. This phenomena is called the belt of Venus

Alex Tudorica

PIX4654264

 
Noctulescent clouds, Venus et Mars - Noctilucent clouds, Venus and Mars - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on June 24, 2009 in Ploumanac'h (Cotes d'Armor). On the right, between the two columns, the planets Venus and Mars. These high altitude clouds are usually seen in summer months but nearer the poles than France. At right, between the two columns, planets Venus and Mars. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

Laurent Laveder

PIX4587791

Noctulescent clouds, Venus et Mars - Noctilucent clouds, Venus and Mars - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on June 24, 2009 in Ploumanac'h (Cotes d'Armor). On the right, between the two columns, the planets Venus and Mars. These high altitude clouds are usually seen in summer months but nearer the poles than France. At right, between the two columns, planets Venus and Mars. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

Laurent Laveder

PIX4587791

 
Aurora Borealis, 1891 (engraving)

Jaime Abecasis

JAB8330761

Aurora Borealis, 1891 (engraving)

Jaime Abecasis

JAB8330761

 
Distorted Moonrise

PIX5619685

Distorted Moonrise

PIX5619685

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