Weather Alert in Texas
Flood Advisory issued April 27 at 8:31PM CDT until April 28 at 1:00PM CDT by NWS Norman OK
AREAS AFFECTED: Wilbarger, TX
DESCRIPTION: ...The National Weather Service in Norman has issued a Flood Advisory for the following rivers in Texas... Pease River near Vernon affecting Wilbarger County. * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Pease River near Vernon. * WHEN...From this evening to early tomorrow afternoon. * IMPACTS...At 14.0 feet, Near bankfull conditions extend along the Pease River in northern Wilbarger County. * ADDITIONAL DETAILS... - At 8:00 PM CDT Sunday the stage was 14.2 feet. - Bankfull stage is 15.0 feet. - Forecast...The Pease River may briefly reach 15 feet overnight before falling - Action stage is 13.0 feet. - Flood stage is 15.0 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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