Night-shining clouds are extremely sensitive to changes in atmospheric water vapor and temperature. The clouds form only when temperatures drop below minus 200 degrees Fahrenheit (minus 130 degrees Celsius), when the scant amount of water high in the atmosphere freezes into ice clouds. This happens most often in far northern and southern latitudes (above 50 degrees) in the summer when, counter-intuitively, the mesosphere is coldest. Changes in temperature or humidity in the mesosphere make the clouds brighter and more frequent. Colder temperatures allow more water to freeze, while an increase in water vapor allows more ice clouds to form. Increased water vapor also leads to the formation of larger ice particles that reflect more light.
The fact that night-shining clouds are getting brighter suggests that the mesosphere is getting colder and more humid, DeLand said. Increasing greenhouse gases in the atmosphere could account for both phenomena.
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Wednesday, February 2, 2011
Noctilucent clouds: There's more of 'em and they're brighter too!
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