Weather Alert in North Carolina
Flood Watch issued July 6 at 1:37AM EDT until July 7 at 8:00AM EDT by NWS Blacksburg VA
AREAS AFFECTED: Stokes; Rockingham; Caswell; Halifax
DESCRIPTION: Tropical Storm Chantal will make landfall early this morning. As the system moves inland, it will spread moderate to heavy rain into the parts of the Piedmonts of Virginia and North Carolina. Between 1 and 2 inches of rain with locally higher amounts are expected through Monday morning. This will cause rises on area rivers and streams, possibly causing flooding. * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Portions of north central North Carolina, including the following counties, Caswell, Rockingham and Stokes and south central Virginia, including the following county, Halifax. * WHEN...From 1 PM EDT this afternoon through Monday morning. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Creeks and streams may rise out of their banks. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - Between 1 and 2 inches of rain with locally higher amounts are expected through Monday morning. - 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 is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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