stratocumulus

As nouns the difference between cumulus and stratocumulus

is that cumulus is a large white puffy cloud that develops through convection on a hot, humid day, they can form towers and even become cumulonimbus clouds while 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.

is likely misspelled.

has no English definition.

As a noun stratocumulus

is 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.

As nouns the difference between taxonomy and stratocumulus

is that taxonomy is the science or the technique used to make a classification while 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.

As nouns the difference between stratocumulus and cumulostratus

is that stratocumulus is 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 cumulostratus is stratocumulus.

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

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 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 stratocumulus and lenticularis

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 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.

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

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 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 stratocumulus and floccus

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 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.

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.