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Engraving depicting a ship amidst a storm from Meteorologia philosophico-politica by Franz Reinzer
Ancient Greece: Life in the country, 1866 (coloured engraving)
'Bad weather
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Instruments of meteorology
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radiosonde investigation balloon used in meteorology
'Diagram of meteorology', 1846
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Diagram of Meteorology, 1846
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'Diagram of meteorology' , 1846
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Meteorology, 1960 (photo)
Clouds at sunset - Clouds in sunse
Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009
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 under angles between 30 and 45* around the antisolar point (at the opposite of the Sun). Then the colors mixe and one can see a white light bow, with sometime blue in the interior and red in the exterior, larger than a rainbo
Cumulonimbus - Cumulonimbus - Light games in a storm cloud.
Cumulus - Cumulus cloud
Ms 624/1596, fol.17r, Compass Rose, from 'Liber Floridus' by Lambert de Saint-Omer, c.1448 (vellum)
Mother-of-pearl cloud - Nacreous clouds - Mother-of-pearl cloud observed in Lapland. Nacreous cloud (or polar stratospheric cloud) seen in Lapland, Finland
Meteorology: the formation of clouds, drawing
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Cloudy sky - Cloudy sky - Cloud formation in Iceland
Cumulonimbus seen from space, Cumulonimbus seen from ISS (photo)
Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009
Anticrepuscular rays - Anticrepuscular rays - Crepuscular rays opposite the sun. Chile. Crepuscular rays seen opposite the sun in the sky. Chile
Earth: clouds and atmosphere - June 2019.
Pearl clouds, Norway, 2020 (photo)
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
Arc circumzenithal - Circumzenithal arc - Arc circumzenithal observed on July 30, 2009. Circumzenithal arc. July 30 2009
Rainbow - Rainbow - Detail of a rainbow with supernumerary arches. Detail of a rainbow with supernumerary rainbow. July 11, 2008
Pearl clouds, Norway, 2020 (photo)
Stormy night - Lightnin
Rainbow Rainbow Panoramic of 6 Vertically Assembled Photos
Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008
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
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
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
Cirrus clouds - floccus species against a pale blue sky
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barometer is a scientific instrument used in meteorology
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
Cover to a work on meteorology and climatology, 1891
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Multiple lightning strikes during a night-time thunderstorm.
Blood rain, miniature of a 10th century Greek manuscript. Biblioteca Marciana, Venice.
Satellite Global Precipitation Measurement (GPM Core Observatory): Artist's view of Global Precipitation Measurement (GPM) satellite in orbit around the Earth. This satellite, launched on 27 February 2014, is dedicated to the study of precipitations (rain and snow) on Earth - Global Precipitation Measurement (GPM) is an international satellite mission to provide next-generation observations of rain and snow worldwide every three hours. NASA and the Japanese Aerospace Exploration Agency (JAXA) launched the GPM Core Observatory satellite on February 27th, 2014, carrying advanced instruments that set a new standard for precipitation measurements from space
Satellite Eole ADM - Aeolus - Artist view - The ADM - Aeolus satellite - Artist view - Artist view of the European satellite Eole ADM - Aeolus (Atmospheric Dynamics Mission) in orbit around the Earth. Using a laser, it will accurately study winds and clouds and increase the accuracy of meteorological forecasts. Its launch is scheduled for 2011. Artist view of the European ADM - Aeolus (Atmospheric Dynamics Mission) satellite in Earth orbit. Equipped with a laser it will provide global observations of wind profiles from space to improve the quality of weather forecasts, and to advance our understanding of atmospheric dynamics and climate processes. Launching scheduled in 2011
Satellite METOP - A - Artist's view of the European satellite METOP - A in orbit around the Earth. Launch on October 19, 2006, it is the first European meteorological satellite in polar orbit; it includes twelve meteorological instruments. MetOp is a series of three meteorological operational polar orbiting satellites, the first of which, MetOp-1 is the prototype. The instruments on MetOp will produce high - resolution images, vertical temperature and humidity profiles, and temperatures of the land and ocean surface on a global basis. Also on board the satellites will be instruments for monitoring ozone and wind flow over the oceans. The first launch was on October 19 2006
Cumulonimbus mammatus - Mammatus nail
Pearl clouds in Oslo, Norway, 2020 (photo)
Rainbow Rainbow Rainbow Rainbow July 11, 2008 Rainbow July 11, 2008
Storm under the stars - Lightning under the stars - A thunderstorm eclate at the tombee of the night
Rainbow on the Great Ocean Road - Rainbow seen while driving on the Great Ocean Road, Victoria, Australia on Jun 11, 2011
Model of 19th century mercury barometers.
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
Storm under the stars: Cumulo-Nimbus, part of a cevenole episode, located about 280 km from the observatory of the Pic du Midi