Weather Alert in North Carolina
Flood Advisory issued August 2 at 4:47PM EDT until August 2 at 7:15PM EDT by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Haywood, NC
DESCRIPTION: * WHAT...Small stream flooding caused by excessive rainfall is expected. * WHERE...A portion of western North Carolina, including the following county, Haywood. * WHEN...Until 715 PM EDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. River or stream flows are elevated. * ADDITIONAL DETAILS... - At 436 PM EDT, Doppler radar indicated heavy rain due to thunderstorms. Minor flooding is ongoing or expected to begin shortly in the Advisory area. Between 1 and 3 inches of rain has fallen over the area with additional rain likely over the next few hours. - This includes the following streams and drainages... Cataloochee Creek, Cold Springs creek, Gunter Fork, Pigeon River, Spring Creek, Hurricane Creek, Chestnut Branch, Andy Branch, Little Cataloochee Creek, Lost Bottom Creek, Big Creek, Dry Branch, Mouse Creek, Dogwood Flats Creek, Balsam Corner Creek, Laurel Branch, Palmer Creek and Mount Sterling Creek. - http://www.weather.gov/safety/flood
INSTRUCTION: When it is safe to do so, please report flooding or landslides threatening roads or property to the National Weather Service Greenville-Spartanburg by calling toll free, 1, 800, 2 6 7, 8 1 0 1, by posting on our Facebook page, or via X using hashtag NWSGSP. Your message should describe the specific location where impacts occurred and the depth of flooding observed.
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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