Weather Alert in Texas
Flood Warning issued April 29 at 8:16PM CDT by NWS Norman OK
AREAS AFFECTED: Wichita, TX; Wilbarger, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Beaver Creek near Electra affecting Wichita and Wilbarger Counties. * WHAT...Major flooding is forecast. * WHERE...Beaver Creek near Electra. * WHEN...From Wednesday evening until further notice. * IMPACTS...At 29.0 feet, Widespread flood levels up to 5 feet in depth cover farm and range lands... and may inundate some oil and gas facilities... along and near the creek in southern Wilbarger County and southwestern Wichita County. * ADDITIONAL DETAILS... - At 8:00 PM CDT Tuesday the stage was 12.1 feet. - Bankfull stage is 24.0 feet. - Forecast...The river will rise above flood stage tomorrow evening to 29.0 feet early Thursday afternoon. - Flood stage is 24.0 feet. - Flood History...This crest compares to a previous crest of 29.0 feet on 04/20/1990. - 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 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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