Weather Alert in North Carolina

Recent Locations: Lewisville, NC  

Flash Flood Warning issued July 6 at 6:56PM EDT until July 7 at 12:45AM EDT by NWS Raleigh NC

AREAS AFFECTED: Moore, NC

DESCRIPTION: FFWRAH The National Weather Service in Raleigh has issued a * Flash Flood Warning for... A Dam Failure of a farm pond at the head of Joes Fork in... Central Moore County in central North Carolina... * Until 1245 AM EDT. * At 656 PM EDT, local law enforcement reported the imminent failure of the farm pond dam. HAZARD...Life threatening flash flooding from the imminent failure of a farm Pond a the head of Joes Fork. SOURCE...Law enforcement reported. IMPACT...Life threatening flash flooding possible for areas downstream from the farm pond at the head of Joes Fork. * The nearest downstream location is Main Street between Richmond St and Alston Dr in Taylortown. Roads along and adjacent to Joes Fork may become flooded and impassable.

INSTRUCTION: If you are in low lying areas along Joes Creek between Taylortown and Whispering Pines you should move to higher ground immediately. Never drive through flooded areas.

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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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