castellanus

As nouns the difference between terms and castellanus

is that terms is while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As a noun castellanus is

(meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As nouns the difference between castellanus and castellans

is that castellanus is a cloud species which shows vertical formations giving a crenellated appearance. Associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera while castellans is plural of lang=en.

In meteorology|lang=en terms the difference between stratocumulus and castellanus

is that stratocumulus is (meteorology) a principal low-level cloud type, predominantly stratiform, in the form of a gray and/or whitish layer or patch, which nearly always has dark parts and is nonfibrous while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As nouns the difference between stratocumulus and castellanus

is that stratocumulus is (meteorology) a principal low-level cloud type, predominantly stratiform, in the form of a gray and/or whitish layer or patch, which nearly always has dark parts and is nonfibrous while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As nouns the difference between altocumulus and castellanus

is that altocumulus is a principal medium-level cloud type, white and/or gray in color, which occurs as a layer or patch with a waved aspect, the elements of which appear as laminae, rounded masses, or rolls. These elements usually are sharply outlined, but they may become partly fibrous or diffuse; they may or may not be merged; they generally have shadowed parts; and, by convection, when observed at an angle of more than 30° above the horizon, subtend an angle between 1 degrees and 5 degrees. (Abbreviated Ac. while castellanus is a cloud species which shows vertical formations giving a crenellated appearance. 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.

In meteorology|lang=en terms the difference between cirrus and castellanus

is that cirrus is (meteorology) a principal high-level cloud type characterised by white, delicate filaments or wisps, of white (or mostly white) patches, or of narrow bands, found at an altitude of above 7000 metres while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As nouns the difference between cirrus and castellanus

is that cirrus is (botany) a tendril while castellanus is (meteorology) a cloud species which shows vertical formations giving a crenellated appearance associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.

As a verb crenellated

is past tense of crenellate.

As an adjective crenellated

is having crenellations or battlements.

As a noun castellanus is

a cloud species which shows vertical formations giving a crenellated appearance. Associated with cirrus, cirrocumulus, altocumulus, and stratocumulus genera.