Weather Alert in North Carolina
Flood Warning issued August 13 at 5:43PM EDT by NWS Wilmington NC
AREAS AFFECTED: Brunswick, NC; Columbus, NC; Horry, SC
DESCRIPTION: ...The Flood Warning is extended for the following rivers in North Carolina... Cape Fear River At William O Huske Lock And Dam 3 affecting Bladen and Cumberland Counties. ...The Flood Warning continues for the following rivers in South Carolina...North Carolina... Waccamaw River At Conway affecting Horry County. Waccamaw River near Longs affecting Horry, Brunswick and Columbus Counties. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Waccamaw River near Longs. * WHEN...Until further notice. * IMPACTS...At 13.0 feet, A few homes may be isolated by flood waters near the river at the end of Big Gutter Lane and Doodle Hill Lane. Flooding on Red Bluff Road worsens. The end of Vera Lane may be isolated by flood waters. Aberdeen Country Club parking lot may flood. In North Carolina, River Road in Pireway may begin to flood. * ADDITIONAL DETAILS... - At 5:00 PM EDT Wednesday the stage was 12.4 feet. - Forecast...The river is expected to rise to a crest of 12.6 feet tomorrow evening. - Flood stage is 12.0 feet. - weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Caution is urged when walking near riverbanks. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Additional information is available at water.noaa.gov/wfo/ilm . The next statement will be issued by Thursday morning.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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