Weather Alert in North Carolina
Flash Flood Warning issued August 20 at 4:02PM EDT until August 20 at 10:00PM EDT by NWS Blacksburg VA
AREAS AFFECTED: Alleghany, NC; Ashe, NC; Watauga, NC; Wilkes, NC; Grayson, VA
DESCRIPTION: FFWRNK The National Weather Service in Blacksburg has issued a * Flash Flood Warning for... Alleghany NC County in northwestern North Carolina... Ashe County in northwestern North Carolina... Southeastern Watauga County in northwestern North Carolina... Central Wilkes County in northwestern North Carolina... Southern Grayson County in southwestern Virginia... * Until 1000 PM EDT. * At 402 PM EDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Between 2 and 3 inches of rain have fallen. 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... Boone... Sparta... Jefferson... West Jefferson... Blowing Rock... Independence... Lansing... This includes the following streams and drainages... Brush Creek, Beaverdam Creek, Bridle Creek, Bee Tree Branch, Bear Branch, Big Sandy Creek, Beaver Creek, Big Pine Creek, Big Horse Creek and Basin Creek.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. When it is safe to do so, please send your reports of flooding, including mudslides or flooded roads, to the National Weather Service by calling toll free at 1...8 6 6...2 1 5...4 3 2 4. Reports and pictures can also be shared on the National Weather Service Blacksburg Facebook page and on X.
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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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