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'Stratus Clouds' images and/or videos results

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Images of 'Stratus Clouds' found, 73

 
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. To the top left of the halo, a halo circumscribed. 26 April 2008, Finistere. 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. A circumscribed halo is also visible towards top left. April 26, 2008

Laurent Laveder

PIX4671000

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. To the top left of the halo, a halo circumscribed. 26 April 2008, Finistere. 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. A circumscribed halo is also visible towards top left. April 26, 2008

Laurent Laveder

PIX4671000

 
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 cause a perfect circle around the Moon. The planets Jupiter and Saturn are also discernible. Image obtained on December 1, 2001. 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. Here are also visible planets Jupiter and Saturn as faint white dots. 1st december 2001

Laurent Laveder

PIX4671695

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 cause a perfect circle around the Moon. The planets Jupiter and Saturn are also discernible. Image obtained on December 1, 2001. 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. Here are also visible planets Jupiter and Saturn as faint white dots. 1st december 2001

Laurent Laveder

PIX4671695

 
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 cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. 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. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004

Laurent Laveder

PIX4671692

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 cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. 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. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004

Laurent Laveder

PIX4671692

 
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 cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 1, 2004. 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. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 1st october 2004

Laurent Laveder

PIX4671681

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 cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 1, 2004. 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. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 1st october 2004

Laurent Laveder

PIX4671681

 
Halo around the Sun and condensation train - Sun Halo and contrail. - 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. A succession of images showing the evolution of the condensation train left by the passage of an aircraft. 14 May 2006, Quimper. 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. Series showing the shift of a contrail and the relative move of its shadow. May 14, 2006

Laurent Laveder

PIX4671004

Halo around the Sun and condensation train - Sun Halo and contrail. - 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. A succession of images showing the evolution of the condensation train left by the passage of an aircraft. 14 May 2006, Quimper. 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. Series showing the shift of a contrail and the relative move of its shadow. May 14, 2006

Laurent Laveder

PIX4671004

 
Dramatic sunset sky over Pladda Island and Ailsa Craig volcanic plug, seen across the sea from Isle of Arran, Scotland, UK (photo)

Chinch Gryniewicz

POV3594364

Dramatic sunset sky over Pladda Island and Ailsa Craig volcanic plug, seen across the sea from Isle of Arran, Scotland, UK (photo)

Chinch Gryniewicz

POV3594364

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the left of the Sun, a brilliant parhely but little colour. - on the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - on the left, the arc of Parry. - near the zenith, the arc circumzenithal, colour. 28 October 2006, Quimper O 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the left of the Sun, a bright parhelia uncolored. - atop the 22* halo, the upper tangent arc. - on the left, the Parr

Laurent Laveder

PIX4670945

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the left of the Sun, a brilliant parhely but little colour. - on the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - on the left, the arc of Parry. - near the zenith, the arc circumzenithal, colour. 28 October 2006, Quimper O 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the left of the Sun, a bright parhelia uncolored. - atop the 22* halo, the upper tangent arc. - on the left, the Parr

Laurent Laveder

PIX4670945

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenitha

Laurent Laveder

PIX4670923

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenitha

Laurent Laveder

PIX4670923

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenitha

Laurent Laveder

PIX4670932

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenitha

Laurent Laveder

PIX4670932

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the left of the Sun, a brilliant parhely but little colour. - on the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - on the left, the arc of Parry. - near the zenith, the arc circumzenithal, colour. 28 October 2006, Quimper O 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the left of the Sun, a bright parhelia uncolored. - atop the 22* halo, the upper tangent arc. - on the left, the Parr

Laurent Laveder

PIX4670954

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the left of the Sun, a brilliant parhely but little colour. - on the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - on the left, the arc of Parry. - near the zenith, the arc circumzenithal, colour. 28 October 2006, Quimper O 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the left of the Sun, a bright parhelia uncolored. - atop the 22* halo, the upper tangent arc. - on the left, the Parr

Laurent Laveder

PIX4670954

 
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

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the right of the Sun, a brilliant parhely but little colour. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele””” to the halo of 22* radius, the arc of Parry. - near the zenith, the cirucmzenithal arc, very colorful. - just in below, tangent and very discreet, l'arc supralateral. 28 October 2006, Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the

Laurent Laveder

PIX4670921

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the right of the Sun, a brilliant parhely but little colour. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele””” to the halo of 22* radius, the arc of Parry. - near the zenith, the cirucmzenithal arc, very colorful. - just in below, tangent and very discreet, l'arc supralateral. 28 October 2006, Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the

Laurent Laveder

PIX4670921

 
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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the right of the Sun, a brilliant parhely but little colour. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele””” to the halo of 22* radius, the arc of Parry. - near the zenith, the cirucmzenithal arc, very colorful. - just in below, tangent and very discreet, l'arc supralateral. 28 October 2006, Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the

Laurent Laveder

PIX4670979

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. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - on the right of the Sun, a brilliant parhely but little colour. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele””” to the halo of 22* radius, the arc of Parry. - near the zenith, the cirucmzenithal arc, very colorful. - just in below, tangent and very discreet, l'arc supralateral. 28 October 2006, Quimper 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. In brief: - around the Sun, the 22* halo, not very contrasted. - on the

Laurent Laveder

PIX4670979

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