Weather Alert in North Carolina
Flood Advisory issued August 14 at 5:08AM EDT until August 14 at 11:15AM EDT by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Henderson, NC; Transylvania, NC
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...A portion of western North Carolina, including the following counties, Henderson and Transylvania. * WHEN...Until 1115 AM EDT Thursday. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 506 AM EDT, At 430 AM EDT, the gauge on Mud Creek had a stage of 12.7 feet. Common, nuisance flooding of low-lying areas adjacent to Mud Creek is ongoing. The lowest elevations of William H King Memorial Park are beginning to flood and floodwaters are approaching the lowest elevations of the Oklawaha Greenway. At this stage, more expansive lowland flooding with nuisance impacts to adjacent farmland, golf courses, and nurseries is ongoing or has recently occurred upstream closer to Erkwood Drive. Although heavy rainfall has ended, the creek level will remain nearly steady early this morning, then slowly fall through late morning. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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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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