Weather Alert in North Carolina
Flood Warning issued July 16 at 10:34AM EDT until July 21 at 2:00PM 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 late tonight to early Monday afternoon. * IMPACTS...At 42.0 feet, Water levels will top the navigational lock and equipment must be removed. Minor flooding will occur on land adjacent to the east bank of the river. * ADDITIONAL DETAILS... - At 10:00 AM EDT Wednesday the stage was 40.4 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight to a crest of 42.7 feet tomorrow evening. It will then fall below flood stage Sunday evening. - Flood stage is 42.0 feet. - weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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 are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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