Weather Alert in Texas
Flood Warning issued April 29 at 2:13PM CDT until May 1 at 5:57AM CDT by NWS Norman OK
AREAS AFFECTED: Baylor, TX; Knox, TX
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Warning for the following rivers in Texas... Brazos River at Seymour affecting Baylor and Knox Counties. * WHAT...Minor flooding is forecast. * WHERE...Brazos River at Seymour. * WHEN...From Wednesday morning to early Thursday morning. * IMPACTS...At 13.0 feet, Short duration flooding affects low-lying areas along and near the river in southern Knox and southern Baylor counties. * ADDITIONAL DETAILS... - At 1:45 PM CDT Tuesday the stage was 2.3 feet. - Bankfull stage is 12.0 feet. - Forecast...The river will rise above flood stage late tomorrow morning to 13.4 feet tomorrow evening. - Flood stage is 12.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Stay tuned to further developments by listening to your local radio, television, or NOAA Weather Radio for further information. Additional information is available at www.weather.gov.
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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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