Weather Alert in Texas
Flood Advisory issued August 29 at 1:24PM CDT until August 29 at 3:15PM CDT by NWS Shreveport LA
AREAS AFFECTED: Gregg, TX; Harrison, TX; Marion, TX; Upshur, TX
DESCRIPTION: * WHAT...Flooding continues caused by earlier excessive heavy rainfall. * WHERE...A portion of northeast Texas, including the following counties, Gregg, Harrison, western Marion and Upshur. * WHEN...Until 315 PM CDT. * IMPACTS...Flooding in low-lying and poor drainage areas. Water over roadways. * ADDITIONAL DETAILS... - At 121 PM CDT, While the heavy rainfall has ended across the advisory area, Doppler radar indicated widespread 2 to 6 inches of rain with isolated higher amounts has fallen. Overflowing poor drainage areas have already caused flooding in the advisory area. - Flooding impacts will continue, but no additional rainfall is expected. - Some locations that will experience flooding include... Longview, Marshall, Kilgore, White Oak, Gladewater, Gilmer, Hallsville, Ore City, Clarksville City, East Mountain, Harleton, Diana, Cedar Springs, West Mountain, Woodlawn, Liberty City, Elysian Fields, Lakeport, Scottsville and Union Grove. - 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 are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
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.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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