Weather Alert in North Carolina
Flood Watch issued May 13 at 3:27PM EDT until May 14 at 2:00AM EDT by NWS Wakefield VA
AREAS AFFECTED: Northampton; Hertford; Gates; Bertie; Chowan; Perquimans; Fluvanna; Prince Edward; Cumberland; Goochland; Mecklenburg; Lunenburg; Nottoway; Amelia; Powhatan; Brunswick; Dinwiddie; Prince George; Greensville; Sussex; Southampton; Western Louisa; Eastern Louisa; Western Hanover; Western Chesterfield; Eastern Chesterfield (Including Col. Heights); Western Henrico (Including the City of Richmond); Eastern Henrico
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of northeast North Carolina, including the following areas, Bertie, Chowan, Gates, Hertford, Northampton and Perquimans and Virginia, including the following areas, Amelia, Brunswick, Cumberland, Dinwiddie, Eastern Chesterfield (Including Col. Heights), Eastern Henrico, Eastern Louisa, Fluvanna, Goochland, Greensville, Lunenburg, Mecklenburg, Nottoway, Powhatan, Prince Edward, Prince George, Southampton, Sussex, Western Chesterfield, Western Hanover, Western Henrico (Including the City of Richmond) and Western Louisa. * WHEN...Until 2 AM EDT Wednesday. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - A period of showers with a few embedded thunderstorms will lead to additional rainfall totals up to 1.5" with locally higher amounts in heavier banding of showers and thunderstorms through late tonight. - 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 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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