Altostratus cloud

From Freepedia

Altostratus is a cloud belonging to a class characterized by a generally uniform gray sheet or layer, lighter in color than nimbostratus and darker than cirrostratus. Compare also with lower altitude stratus clouds.

Altostratus
Where found: 2,000-5,000 m
Associated weather: Wide areas of rain and snow.

Altostratus is caused by a large air mass that is lifted then condensed, usually by an incoming frontal system.

Altostratus clouds are potentially dangerous, because they can cause ice accretion on aircraft.

Bold text

External links

Wikimedia Commons has more media related to:
[[Commons:Category:{{{1|Altostratus cloud}}}|{{{1|Altostratus cloud}}}]]


Views
Personal tools
In other languages
Similar Links