Weather Alert in Texas
Flood Watch issued April 29 at 8:24AM CDT until May 1 at 8:39AM CDT by NWS Norman OK
AREAS AFFECTED: Knox; Baylor
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Watch for the following rivers in Texas... Brazos River at Seymour affecting Baylor and Knox Counties. * WHAT...Flooding is possible. * WHERE...Brazos River at Seymour. * WHEN...From Wednesday morning to 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 7:45 AM CDT Tuesday the stage was 2.3 feet. - Forecast...Flood stage may be reached late tomorrow morning. - Flood stage is 12.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. 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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