How do cirrocumulus clouds influence weather?

A cirrocumulus cloud is often a cloud formed by a cumulus that rose along a warm from and is now like a thin veil right under the tropopause, entirely made of ice crystals. read more

A cirrocumulus cloud is often a cloud formed by a cumulus that rose along a warm from and is now like a thin veil right under the tropopause, entirely made of ice crystals. As any other cloud, their albedo reduces the sun’s energy reaching the ground. read more

Cirrocumulus is one of the three main genus-types of high-altitude tropospheric clouds, the other two being cirrus and cirrostratus. They usually occur at an altitude of 5 kilometres (16,000 ft) to 12 kilometres (39,000 ft). Like lower altitude cumuliform and stratocumuliform clouds, cirrocumulus signifies convection. read more

Precipitation from cirrocumulus clouds never reaches the surface, meaning that these clouds are usually associated with fair-weather. However their appearance can often prelude stormy weather meaning you should make the most of the sun while you still can. read more

Cirrocumulus (Cc) - the name is a composite of the Latin cirrus = wisp or curl and cumulus = small heap. Cirrocumulus is a member of the ten fundamental cloud types (or cloud genera). Cirrocumuli are high-level clouds appearing as a formation of small masses of white or pale blue, fleecy clouds in a globular, wavelike, rippled pattern, usually in regularly arranged groupings. read more

Cirrocumulus is one of the three main genus-types of high-altitude tropospheric clouds, the other two being cirrus and cirrostratus.[3] They usually occur at an altitude of 5 kilometres (16,000 ft) to 12 kilometres (39,000 ft). read more