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.