Weather Alert in North Carolina
Flood Warning issued August 13 at 10:07PM EDT until August 17 at 2:00AM EDT by NWS Newport/Morehead City NC
AREAS AFFECTED: Greene, NC; Lenoir, NC; Pitt, NC
DESCRIPTION: ...The Flood Warning continues for the following rivers in North Carolina... Contentnea Creek Near Hookerton affecting Greene, Lenoir and Pitt Counties. For the Contentnea Creek...including Hookerton...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Contentnea Creek near Hookerton. * WHEN...From late tonight to early Sunday morning. * IMPACTS...At 13.0 feet, Minor flooding of low lying areas adjacent to creek can be expected. Several homes threatened by water in northwest Greene County near HWY 58. * ADDITIONAL DETAILS... - At 9:00 PM EDT Wednesday the stage was 12.9 feet. - Forecast...The river is expected to rise above flood stage just after midnight tonight to a crest of 13.2 feet tomorrow evening. It will then fall below flood stage Saturday evening. - Flood stage is 13.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at water.weather.gov/ahps. The next statement will be issued Thursday afternoon at 415 PM EDT.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
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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