Weather Alert in Texas
Flood Advisory issued July 4 at 3:47PM CDT until July 4 at 7:00PM CDT by NWS Austin/San Antonio TX
AREAS AFFECTED: Gillespie, TX; Kerr, TX
DESCRIPTION: * WHAT...Urban and small stream flooding caused by excessive rainfall is expected. * WHERE...A portion of south central Texas, including the following counties, Gillespie and Kerr. * WHEN...Until 700 PM CDT. * IMPACTS...Dangerous flows over low-water crossings. Water over roadways. Some low-water crossings may become impassable. * ADDITIONAL DETAILS... - At 347 PM CDT, Doppler radar and automated rain gauges indicated heavy rain due to thunderstorms. This will cause urban and small stream flooding. Between 2 and 7 inches of rain have fallen. - Additional rainfall amounts up to 1 inch are expected over the area. - Some locations that will experience flooding include... Fredericksburg, Stonewall, Tivydale, Harper, Doss, Cherry Spring, Mountain Home, Cain City, Grapetown, Crabapple, Rocky Hill, Luckenbach, Enchanted Rock State Natural Area, Blumenthal, Eckert, Kerr Wildlife Management Area, Willow City, LBJ State Park, Albert and LBJ National Historical Park. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads.
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Weather Topic: What is Snow?
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Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
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Weather Topic: What are Stratus Clouds?
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Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
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