cirrocumulus

As a noun cirrocumulus is

(physics|meteorology) a principal high-level cloud type appearing as a thin, white patch of cloud without shadows, composed of very small droplets in the form of grains or ripples the elements may be merged or separate, and more or less regularly arranged; they subtend an angle of less than 1° when observed at an angle of more than 30° above the horizon holes or rifts often occur in a sheet of cirrocumulus abbreviated cc.

As nouns the difference between cirrostratus and cirrocumulus

is that cirrostratus is (meteorology) a principal high-level cloud type appearing as a whitish veil, usually fibrous but sometimes smooth, which may totally cover the sky and which often produces halo phenomena, either partially or completely sometimes a banded aspect may appear, but the intervals between the bands are filled with thinner cloud veil the edge of the veil of cirrostratus may be straight and clean-cut, but more often it is irregular and fringed with cirrus some of the ice crystals that comprise the cloud are large enough to fall and thereby produce a fibrous aspect cirrostratus occasionally may be so thin and transparent as to render it almost indiscernible, especially through haze or at night at such times, the existence of a halo may be the only revealing feature, such as producing a halo around the moon abbreviated: cs while cirrocumulus is (physics|meteorology) a principal high-level cloud type appearing as a thin, white patch of cloud without shadows, composed of very small droplets in the form of grains or ripples the elements may be merged or separate, and more or less regularly arranged; they subtend an angle of less than 1° when observed at an angle of more than 30° above the horizon holes or rifts often occur in a sheet of cirrocumulus abbreviated cc.

As nouns the difference between cirrocumulus and lenticularis

is that cirrocumulus is (physics|meteorology) a principal high-level cloud type appearing as a thin, white patch of cloud without shadows, composed of very small droplets in the form of grains or ripples the elements may be merged or separate, and more or less regularly arranged; they subtend an angle of less than 1° when observed at an angle of more than 30° above the horizon holes or rifts often occur in a sheet of cirrocumulus abbreviated cc while lenticularis is (meteorology) a cloud species which consists of rounded lens shaped of cloud, often forming near mountains associated with cirrocumulus, and altocumulus, and sometimes stratocumulus genera.

As nouns the difference between cirrocumulus and floccus

is that cirrocumulus is (physics|meteorology) a principal high-level cloud type appearing as a thin, white patch of cloud without shadows, composed of very small droplets in the form of grains or ripples the elements may be merged or separate, and more or less regularly arranged; they subtend an angle of less than 1° when observed at an angle of more than 30° above the horizon holes or rifts often occur in a sheet of cirrocumulus abbreviated cc while floccus is (meteorology) a cloud species which consists of rounded tufts of cloud, often formed by dissipation from larger cloud species associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As nouns the difference between cirrocumulus and castellanus

is that cirrocumulus is (physics|meteorology) a principal high-level cloud type appearing as a thin, white patch of cloud without shadows, composed of very small droplets in the form of grains or ripples the elements may be merged or separate, and more or less regularly arranged; they subtend an angle of less than 1° when observed at an angle of more than 30° above the horizon holes or rifts often occur in a sheet of cirrocumulus abbreviated cc while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.