Примери за cirrocumulus

• A few cirrocumulus clouds were coming up from the east when we started, but we left them behind, and nothing was visible during the night but a thin hazy veil. 

• A few cirrocumulus continued to pass over towards east. 

• Towards afternoon, cirrocumulus and cirrostratus began to appear moving northward. 

• It is a fairly uncommon phenomenon, most often observed in altocumulus, cirrocumulus, lenticular clouds and cirrus clouds.

• Cirrocumulus lenticularis forms when stable air is forced upward; this is usually due to orographic features, but can occur away from mountains as well.

• Cirrocumulus clouds never cast self-shadows and are translucent to a certain degree.

• Convection at high altitudes can produce another high-based genus called cirrocumulus, a pattern of small cloud tufts that contain droplets of supercooled water.

• Cirrocumulus castellanus is an indicator of atmospheric instability at the level of the cloud.

• Like cirrocumulus castellanus, cirrocumulus floccus is an indicator of atmospheric instability at the level of the cloud.

• In fact, cirrocumulus floccus can form from cirrocumulus castellanus, being the evolutionary state after the base of the original cloud has dissipated.

• Cirrocumulus are, like other members of the cumuliform and stratocumuliform categories, formed via convective processes.

• The resulting cloud forms may resemble cirrus, cirrocumulus, or cirrostratus, and are sometimes called cirrus aviaticus.

• The other two genera, cirrocumulus and cirrostratus, are also high clouds.

• High-tage tropospheric genus-types, "cirrus", "cirrocumulus", and "cirrostratus", particularly show this duality with both short-wave albedo cooling and long-wave greenhouse warming effects.

• Unlike other high cirrus and cirrostratus, cirrocumulus includes a small amount of liquid water droplets, although these are in a supercooled state.

• Cirrocumulus clouds come in four species: "stratiformis", "lenticularis", "castellanus", and "floccus".

• Cirrocumulus stratiformis occurs as very small cirrocumulus clouds that cover a large part of the sky.

• The high-tage clouds are all cirriform, one of which, cirrocumulus, is also cumuliform of limited convection or stratocumuliform.