Sc (StratoCumulus) formed by the spreading out of cumulus; cumulus may also be present Sc not resulting from the spreading out of cumulus St (Stratus) or Sf (Stratus Fractus) in a more or less continuous sheet or layer, or in ragged shreds, or both, but no stratus fractus of bad weather Stratocumulus: Puffy, low to the ground and very gray, stratocumulus clouds gather in lines. The clouds show little movement, hence the name standing. Stratocumulus castellanus - These are thicker, more drizzly stratocumulus clouds. It is lighter in color than nimbostratus and darker than high cirrostratus.The sun can be seen through thin … A cloud at the surface is called a fog. Low clouds, 2 to 0 km (6,500 to 0 feet), are stratocumulus, stratus, and nimbostratus. Rain rarely occurs with stratocumulus clouds, however, they can turn into nimbostratus clouds. Asperitas (formerly known as Undulatus asperatus) is a cloud formation first popularized and proposed as a type of cloud in 2009 by Gavin Pretor-Pinney of the Cloud Appreciation Society.Added to the International Cloud Atlas as a supplementary feature in March 2017, it is the first cloud formation added since cirrus intortus in 1951. Wind, however, can be quite strong blowing through such clouds. Standing lenticular altocumulus clouds are formed on the crests of waves created by barriers in the wind flow. They are characterized by their smooth, pol ... STRATOCUMULUS. The name translates approximately as "roughness". Altostratus is a middle altitude cloud genus belonging to the stratiform physical category characterized by a generally uniform gray to bluish-green sheet or layer. Most form in rows with blue sky visible in between them. A cloud that extends through all three heights is called a cumulonimbus . Although stratocumulus clouds rarely produce precipitation, they can easily grow into rainy nimbostratus clouds. Hints of blue sky peek out between the rows. Hints of blue sky peek out between the rows. Stratocumulus clouds are low, puffy and gray. Turreted tops form when convection initiates through the stable layer, allowing stratocumulus to grow upwards and potentially leading to the formation of cumulus congestus or even cumulonimbus .
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