Weather Alert in North Carolina

Recent Locations: Bangs, TX   Elmhurst, IL   Dublin, NC  

Special Weather Statement issued February 28 at 10:07PM EST by NWS Wilmington NC

AREAS AFFECTED: Robeson; Marlboro; Darlington; Dillon; Florence; Marion; Williamsburg; Inland Georgetown; Coastal Georgetown

DESCRIPTION: Areas where low clouds persisted during Saturday afternoon will be the prime locations where areas of fog reducing visibility to 1 to 3 miles will develop. Within these areas, locally dense fog is likely that will further reduce visibility to near 0 at times resulting in hazardous driving conditions. The fog will persist into Sunday morning and should disperse by 9 or 10 am the latest.

INSTRUCTION: Motorists encountering the fog should immediately SLOW down, make use of their low beam headlights and allow extra distance between you and the vehicle ahead in case of a sudden stop.

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Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

Stratus Clouds Next Topic: Wall Clouds

Stratus clouds are similar to altostratus clouds, but form at a lower altitude and are identified by their fog-like appearance, lacking the distinguishing features of most clouds.

Stratus clouds are wider than most clouds, and their base has a smooth, uniform look which is lighter in color than a nimbostratus cloud. The presence of a stratus cloud indicates the possibility of minor precipitation, such as drizzle, but heavier precipitation does not typically arrive in the form of a stratus cloud.

Next Topic: Wall Clouds

Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

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