Altocumulus Clouds. This form occurs as a mid-level cloud and appears patchy and puffy in the sky; ... Altostratus clouds form as layers of thin, gray clouds stretching out in sheets across the sky.

Altocumulus clouds occur in a few different types, not just these balls of fluff. ... Stratus clouds are gray layers, sometimes with variances in their luminescence.

Altocumulus: White and gray, patchy clouds that are layered, sheet-like in the sky and generally composed of plates, rounded masses or rolls.

Mid-level clouds are usually gray and are identified as either altocumulus, altostratus, or nimbostratus. Altocumulus clouds are full of liquid water but generally do not produce rain.

The two main types are altostratus and altocumulus. The final cloud class are the low-level clouds, ... Why do clouds turn gray? A cloud gets its bright coloring from the sunlight hitting it.

Clouds that exist in the mid-levels of the atmosphere are between 7-thousand to 23-thousand feet. Clouds are grouped by type and height, so altocumulus are mid-level, grayish-white cumulus clouds.

Altocumulus: White and gray, patchy clouds that are layered, sheet-like in the sky and generally composed of plates, rounded masses or rolls.

Middle clouds: Altostratus, altocumulus and nimbostratus clouds are typically found between 6,000 and 20,000 feet above the ground. Altostratus resembles a smooth gray sheet across the sky.

Stratiformis is another common species of altocumulus, where high clouds appear like a patchy, ridged sheet. Similarly, if there are layers of cloud that cover the sun entirely, they may be a ...

High Clouds (16,500-45,000 feet) These clouds form high up in the atmosphere, and you’ll usually find the Cirrus cloud family here. These clouds are thin, wispy, and often look like strands of ...

Altostratus: Gray or blue-gray clouds that often blanket the sky and obscure the sun, giving the sky a dull appearance. Altocumulus : Puffy, rounded clouds that may appear in groups or waves.

Altocumulus lenticularis – how they form. Lenticular clouds are created when a stable layer of humid air is forced to rise over high ground, condensing its moisture into cloud.