Weather Alert in Oklahoma
Flood Advisory issued June 16 at 2:50AM CDT until June 17 at 7:00AM CDT by NWS Norman OK
AREAS AFFECTED: Comanche, OK; Cotton, OK
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Oklahoma... East Cache Creek near Walters affecting Cotton and Comanche Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...East Cache Creek near Walters. * WHEN...Until tomorrow morning. * IMPACTS...At 18.0 feet, Some inundation of bottomlands may occur along and near the creek in southern Comanche County and Cotton County. * ADDITIONAL DETAILS... - At 2:30 AM CDT Monday the stage was 16.7 feet. - Bankfull stage is 15.0 feet. - Forecast...The East Cache Creek is expected to rise to a crest of 18.0 feet this afternoon. - Action stage is 15.0 feet. - Flood stage is 21.0 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 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
Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
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