Weather Alert in Oklahoma
Flood Warning issued April 29 at 8:14AM CDT until May 3 at 7:25AM CDT by NWS Norman OK
AREAS AFFECTED: Cotton, OK
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Oklahoma... Deep Red Creek near Randlett affecting Cotton County. * WHAT...Minor flooding is occurring and moderate flooding is forecast. * WHERE...Deep Red Creek near Randlett. * WHEN...Until Saturday morning. * IMPACTS...At 26.0 feet, Valley-wide flooding of croplands... pastures... and local roads occurs and is accompanied by flood depths up to 6 feet with dangerous currents. * ADDITIONAL DETAILS... - At 7:30 AM CDT Tuesday the stage was 22.9 feet. - Bankfull stage is 20.0 feet. - Forecast...The Deep Red Creek is expected to rise to a crest of 25.6 feet Thursday morning. It will then fall below flood stage early Saturday morning. - Flood stage is 20.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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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