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Clouds and skyClouds and sky
Terrestrial cloud formation is the result of air in Earth's atmosphere becoming saturated due to either or both of two processes; cooling of the air and adding water vapor. With sufficient saturation, precipitation will fall to the surface; an exception is virga, which evaporates before reaching the surface. Clouds in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard's nomenclature. It was introduced in December 1802 and became the basis of the modern classification system. Synoptic surface weather observations use code numbers to record and report any type of tropospheric cloud visible at scheduled observation times based on its height and physical appearance.
Available online at: http://en.wikipedia.org/wiki/Cloud
Clouds over Setesdalsheia, Norway, October 2013
Clouds over Setesdalsheia, Norway, October 2013
Clouds over Setesdalsheia, Norway, October 2013
Clouds over Setesdalsheia, Norway, October 2013
Clouds over Himalaya, Nepal
Clouds over Himalaya, Nepal
Clouds over Himalaya, Nepal
Clouds over Sahara Desert, Egypt
Clouds over Northern Kenya, October 2013
Clouds over Northern Kenya, October 2013
Clouds over Northern Kenya, October 2013