Weather Alert in North Carolina
Flood Watch issued July 6 at 10:56PM EDT until July 7 at 6:00AM EDT by NWS Raleigh NC
AREAS AFFECTED: Person; Granville; Forsyth; Guilford; Alamance; Orange; Durham; Davidson; Randolph; Chatham; Stanly; Montgomery; Moore; Lee; Anson; Richmond; Scotland; Hoke
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...A portion of central North Carolina, including the following counties, Alamance, Anson, Chatham, Davidson, Durham, Forsyth, Granville, Guilford, Hoke, Lee, Montgomery, Moore, Orange, Person, Randolph, Richmond, Scotland and Stanly. * WHEN...Until 6 AM EDT Monday. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - The remnants of Tropical Depression Chantal will bring widespread showers and embedded storms across central North Carolina through early Monday. Storm total rainfall amounts of 1 to 3 inches are expected, with locally 4 or more inches possible, with the highest totals likely to be in the Piedmont and western Sandhills, along and west of US Highway 1. This rainfall may result in flash flooding. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
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