Weather Alert in North Carolina
Flood Warning issued August 13 at 10:21AM EDT until August 16 at 7:05PM EDT by NWS Wilmington NC
AREAS AFFECTED: Bladen, NC; Cumberland, NC
DESCRIPTION: ...The National Weather Service in Wilmington NC has issued a Flood Warning for the following rivers in North Carolina... Cape Fear River At William O Huske Lock And Dam 3 affecting Bladen and Cumberland Counties. * WHAT...Minor flooding is forecast. * WHERE...Cape Fear River at William O Huske Lock And Dam 3. * WHEN...From this afternoon to Saturday evening. * IMPACTS...At 45.0 feet, Flood waters will affect lowlands along the east bank of the river with some minor overflow along the west bank. * ADDITIONAL DETAILS... - At 9:00 AM EDT Wednesday the stage was 40.9 feet. - Forecast...The river is expected to rise above flood stage late this afternoon to a crest of 44.6 feet tomorrow evening. It will then fall below flood stage early Saturday morning. - Flood stage is 42.0 feet. - weather.gov/safety/flood
INSTRUCTION: 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 late tonight.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
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Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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