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 Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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