Weather Alert in Texas
Flood Advisory issued April 28 at 1:52PM CDT until May 1 at 7:00AM CDT by NWS Norman OK
AREAS AFFECTED: Wichita, TX; Wilbarger, TX
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Texas... Beaver Creek near Electra affecting Wichita and Wilbarger Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Beaver Creek near Electra. * WHEN...Until Thursday morning. * IMPACTS...At 23.0 feet, Shallow and short duration flooding of lowlands along and near the creek may occur in southern Wilbarger County and southwestern Wichita County. * ADDITIONAL DETAILS... - At 1:00 PM CDT Monday the stage was 18.2 feet. - Bankfull stage is 24.0 feet. - Forecast...The Beaver Creek is expected to rise to a crest of 23.0 feet early Wednesday morning. - Action stage is 22.0 feet. - Flood stage is 24.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you encounter a flooded roadway, turn around and find an alternative route. Additional information is available at www.weather.gov.
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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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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