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Images de 'Parhely' médias trouvés, 24

 
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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

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

 
Le partenaire de contenu applique les restrictions suivantes
  • Only available to clients invoiced in Balkans;Only available to clients invoiced in Europe;Only available to clients invoiced in Norway;Only available to clients invoiced in Switzerland
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Parhelie sur Pluto - Artist's view - Parhelie sur Pluto - Artist's view - Artist's view of the icy surface of Pluto and the Sun. When Pluto is at its perihelie, that is to say the closest to the Sun, it has a very fine atmosphere. Some optical phenomena could then occur as here, a parhely

Dixon, Don (b.1951)

PIX4624441

Parhelie sur Pluto - Artist's view - Parhelie sur Pluto - Artist's view - Artist's view of the icy surface of Pluto and the Sun. When Pluto is at its perihelie, that is to say the closest to the Sun, it has a very fine atmosphere. Some optical phenomena could then occur as here, a parhely

Dixon, Don (b.1951)

PIX4624441

 
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. - 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 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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