Weather Alert in North Carolina
Flood Watch issued May 11 at 2:49PM EDT until May 13 at 8:00AM EDT by NWS Greenville-Spartanburg SC
AREAS AFFECTED: Avery; Alexander; Yancey; Mitchell; Southern Jackson; Transylvania; Henderson; Caldwell Mountains; Greater Caldwell; Burke Mountains; Greater Burke; McDowell Mountains; Eastern McDowell; Rutherford Mountains; Greater Rutherford; Polk Mountains; Eastern Polk; Pickens Mountains; Greenville Mountains
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall is possible. * WHERE...Portions of North Carolina, including the following areas, Alexander, Avery, Burke Mountains, Caldwell Mountains, Eastern McDowell, Eastern Polk, Greater Burke, Greater Caldwell, Greater Rutherford, Henderson, McDowell Mountains, Mitchell, Polk Mountains, Rutherford Mountains, Southern Jackson, Transylvania and Yancey and Upstate South Carolina, including the following areas, Greenville Mountains and Pickens Mountains. * WHEN...From Monday morning through Tuesday morning. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - A slow-moving storm system is expected to bring multiple rounds of showers and storms on Monday and Monday night. Runoff from the moderate to heavy rainfall will likely cause flooding. The heaviest rainfall and greatest risk for flash flooding is expected along the Blue Ridge Escarpment and the southern and eastern-facing slopes of the mountains in western North Carolina. Rainfall totals on 3-5 inches with isolated amounts between 6 and 8 inches are possible in these areas. This will not be anywhere near the magnitude of flooding that occurred during Helene. - http://www.weather.gov/safety/flood
INSTRUCTION: A Flood Watch for flash flooding means there is a potential for rapid onset flooding based on current forecasts. Flash flooding is a very dangerous situation and may impact areas that do not typically flood. Please monitor the latest forecasts and be prepared to take action quickly should Flash Flood Warnings be issued. Rainfall of more than five inches in similar storms has been associated with an increased risk of landslides and rockslides. If you live on a mountainside or in a cove at the base of a mountain, especially near a stream, be ready to leave in advance of the storm or as quickly as possible should rising water, moving earth, or rocks threaten. Consider postponing travel along mountain roads during periods of heavy rainfall.
Want more detail? Get the Complete 7 Day and Night Detailed Forecast!
Current U.S. National Radar--Current
The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).
National Weather Forecast--Current
The Current National Weather Forecast and National Weather Map are shown below.
National Weather Forecast for Tomorrow
Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.
North America Water Vapor (Moisture)
This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.
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
Current conditions powered by WeatherAPI.com
