Weather Alert in Texas
Flood Warning issued July 6 at 4:45PM CDT until July 6 at 6:45PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Comanche, TX; Mills, TX
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Portions of Comanche and Mills counties in Central Texas. * WHEN...Until 645 PM CDT. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is ongoing or imminent. * ADDITIONAL DETAILS... - Doppler radar and automated rain gauges indicated heavy rain due to thunderstorms earlier this afternoon. Flooding is ongoing. Up to 2.5 inches of rain have fallen, and light rain will continue for the next couple of hours. - Some locations that will experience flooding include... Comanche, Goldthwaite, Gustine, Proctor Lake, Democrat, Newburg, Priddy, Energy, Hasse, Caradan, Van Dyke, Pecan Wells, Proctor, Lamkin and Bozar.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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