Stratus (St)
CL · Low level · Surface–2,000 m (surface–6,500 ft)
A uniform grey layer with a low, often ragged base; fog that does not touch the ground.
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When the sun is visible through stratus, its outline is sharp — the opposite of altostratus. It forms in gentle lifting of a moist stable layer, or as advection fog lifting off the surface. Hill fog is simply stratus meeting high ground; the same layer overhead gives long dull spells and, at most, drizzle.
Precipitation: Drizzle, snow grains or ice prisms.
Name: stratus — spread out, layered
Photo: Wikimedia Commons
