0 a type of cumulus (= tall, rounded, white cloud with a flat base) formed in a thick layer and found at low height -- 层积云
The low, sharp inversion can lead to areas of persistent stratocumulus or stratus cloud, colloquially known as anticyclonic gloom.
The laboratory results may be related to the behaviour of marine stratocumulus clouds.
This can create the illusion of continuous precipitation of more than very light intensity falling from stratocumulus.
The stability of stratocumulus clouds with strong evaporative cooling effects is explored in laboratory simulations.
Drizzle is normally produced by low stratiform clouds and stratocumulus clouds.
But until the late 1990s, scientists had dismissed them as merely a relatively uncommon transitional form between open- and closed-cell formations of stratocumulus clouds.
Like all other forms of stratocumulus apart from castellanus, they are also often found in anticyclones.
The two genera that are strictly low-tage are stratus, and stratocumulus.
