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'Atmospheric Phenomena' images and/or videos results

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Images of 'Atmospheric Phenomena' found, 169

 
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

 
Double rainbow - rainbow - double rainbow - double rainbow over the hills of Lomagne, Gers, France. Panoramic of 6 images. Double rainbow seen above Lomagne hills, Gers, France. Six panorama images

Patrick Lécureuil

PIX4671219

Double rainbow - rainbow - double rainbow - double rainbow over the hills of Lomagne, Gers, France. Panoramic of 6 images. Double rainbow seen above Lomagne hills, Gers, France. Six panorama images

Patrick Lécureuil

PIX4671219

 
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

 
Moon rainbow in Norway - Lunar Rainbow in Norway

Alex Conu

PIX4634009

Moon rainbow in Norway - Lunar Rainbow in Norway

Alex Conu

PIX4634009

 
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

 
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

 
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

 
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

 
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Sunset at St Germain, c.1940 (oil on board)

Rowntree, Kenneth (1915-97)

LIS2651549

Sunset at St Germain, c.1940 (oil on board)

Rowntree, Kenneth (1915-97)

LIS2651549

 
A 3-section panorama of a retreating thunderstorm, southern Alberta, Canada (photo)

UIG5317197

A 3-section panorama of a retreating thunderstorm, southern Alberta, Canada (photo)

UIG5317197

 
A rainbow near sunset in Alberta, May 31, 2014 (photo)

UIG5317205

A rainbow near sunset in Alberta, May 31, 2014 (photo)

UIG5317205

 
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Lightnings, 1910 (oil on canvas)

Russolo, Luigi (1885-1947)

Alessandro Vasari

MEP2627353

Lightnings, 1910 (oil on canvas)

Russolo, Luigi (1885-1947)

Alessandro Vasari

MEP2627353

 
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Untitled (Cowboy), 1995 (ektacolour print)

Prince, Richard (b.1949)

CH1771204

Untitled (Cowboy), 1995 (ektacolour print)

Prince, Richard (b.1949)

CH1771204

 
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Twilight in Paris (oil on canvas)

Canu, Yvonne (b.1921)

CH1769145

Twilight in Paris (oil on canvas)

Canu, Yvonne (b.1921)

CH1769145

 
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Rainbow, King's Sedgemoor, 2001 (tempera on canvas)

Lynch, James

LYN312044

premium

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Rainbow, King's Sedgemoor, 2001 (tempera on canvas)

Lynch, James

LYN312044

 
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Sadak in Search of the Waters of Oblivion, 1812 (oil on canvas)

Martin, John (1789-1854)

STM620397

Sadak in Search of the Waters of Oblivion, 1812 (oil on canvas)

Martin, John (1789-1854)

STM620397

 
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The Sun and Solar Phenomena', c 1860

UIS5090372

The Sun and Solar Phenomena', c 1860

UIS5090372

 
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The Sun and Solar Phenomena', c 1855

UIS5096262

The Sun and Solar Phenomena', c 1855

UIS5096262

 
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Natural phenomenon, Moscow, Russia, 1812

UIS5096304

Natural phenomenon, Moscow, Russia, 1812

UIS5096304

 
Earth's atmosphere and noctiluque clouds - Earth's atmosphere and noctilucent clouds - View of the Earth's atmosphere with night clouds photographs from the International Space Station on July 22, 2008. These clouds look like cirrus but are much higher, between 75 and 90 km from the Earth's surface. Polar Mesospheric Clouds (also known as noctilucent clouds) are transient, upper atmospheric phenomena observed usually in the summer months at high latitudes (greater than 50 degrees) of both the Northern and Southern Hemispheres. They are bright and cloudlike in appearance while in deep twilight. They are illuminated by sunlight when the lower layers of the atmosphere are in the darkness of the Earth's shadow. This image was acquired at an altitude of just over 200 miles in the pre - dawn hours of July 22, 2008 as the International Space Station was passing over western Mongolia in central Asia. The dark horizon of the Earth appears below with some layers of the lower atmosphere already i

PIX4675175

Earth's atmosphere and noctiluque clouds - Earth's atmosphere and noctilucent clouds - View of the Earth's atmosphere with night clouds photographs from the International Space Station on July 22, 2008. These clouds look like cirrus but are much higher, between 75 and 90 km from the Earth's surface. Polar Mesospheric Clouds (also known as noctilucent clouds) are transient, upper atmospheric phenomena observed usually in the summer months at high latitudes (greater than 50 degrees) of both the Northern and Southern Hemispheres. They are bright and cloudlike in appearance while in deep twilight. They are illuminated by sunlight when the lower layers of the atmosphere are in the darkness of the Earth's shadow. This image was acquired at an altitude of just over 200 miles in the pre - dawn hours of July 22, 2008 as the International Space Station was passing over western Mongolia in central Asia. The dark horizon of the Earth appears below with some layers of the lower atmosphere already i

PIX4675175

 
Distorted Moonrise

PIX5619685

Distorted Moonrise

PIX5619685

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