Weather Alert in Oklahoma
Flood Watch issued August 28 at 2:28AM CDT until August 30 at 4:00PM CDT by NWS Norman OK
AREAS AFFECTED: Grant; Kay; Noble
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Watch for the following rivers in Oklahoma... Salt Fork Arkansas River at Tonkawa affecting Noble, Kay and Grant Counties. * WHAT...Flooding is possible. * WHERE...Salt Fork Arkansas River at Tonkawa. * WHEN...From late tonight to Saturday afternoon. * IMPACTS...At 19.0 feet, Flood depths ranging up to about 2 feet move from eastern Grant County... across Kay County... to the confluence with the Arkansas River below Ponca City. Farmland and oilfields are flooded hours before the crest. * ADDITIONAL DETAILS... - At 1:30 AM CDT Thursday the stage was 4.1 feet. - Forecast...Flood stage may be reached late tonight. - Flood stage is 17.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. 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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