Weather Alert in North Carolina
Flood Warning issued August 11 at 10:49PM EDT until August 13 at 1:21PM EDT by NWS Raleigh NC
AREAS AFFECTED: Johnston, NC
DESCRIPTION: ...The National Weather Service in Raleigh NC has issued a Flood Warning for the following rivers in North Carolina... Neuse River Near Clayton affecting Johnston County. * WHAT...Minor flooding is forecast. * WHERE...Neuse River near Clayton. * WHEN...From late tonight to early Wednesday afternoon. * IMPACTS...At 9.0 feet, Minor flooding begins. Minor overflow occurs on both banks. Water reaches the edge of the Neuse River Greenway trail. At 10.0 feet, Upstream of the gage site, the Neuse River Greenway at Covered Bridge Road begins to flood. * ADDITIONAL DETAILS... - At 10:15 PM EDT Monday the stage was 7.5 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 10.1 feet early tomorrow afternoon. It will then fall below flood stage early Wednesday morning. - Flood stage is 9.0 feet. - water.noaa.gov/gauges/CLYN7
INSTRUCTION: Caution is urged when walking near riverbanks. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov/rah/rivers. The next statement will be issued Tuesday afternoon.
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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
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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.
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