Weather Alert in North Carolina
Flash Flood Warning issued June 13 at 3:40PM EDT until June 13 at 6:30PM EDT by NWS Raleigh NC
AREAS AFFECTED: Harnett, NC; Hoke, NC; Montgomery, NC; Moore, NC; Richmond, NC
DESCRIPTION: FFWRAH The National Weather Service in Raleigh has issued a * Flash Flood Warning for... Southwestern Harnett County in central North Carolina... Northern Hoke County in central North Carolina... Southeastern Montgomery County in central North Carolina... Southern Moore County in central North Carolina... Northeastern Richmond County in central North Carolina... * Until 630 PM EDT. * At 340 PM EDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Between 2 and 3 inches of rain have fallen. Additional rainfall amounts of 1 to 3 inches are possible in the warned area. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. * Some locations that will experience flash flooding include... Southern Pines, Pinehurst, Aberdeen, Hoffman, Whispering Pines, Pinebluff, Ellerbe, Foxfire, Taylortown, Vass, Cameron, Norman, Ashley Heights, Seven Lakes, Sandhills Game Land and Derby.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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