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 Altocumulus Clouds?
Home - Education - Cloud Types - 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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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