Weather Alert in Oklahoma
Flood Advisory issued August 30 at 8:07PM CDT until September 2 at 1:00AM CDT by NWS Norman OK
AREAS AFFECTED: Major, OK; Woods, OK; Woodward, OK
DESCRIPTION: ...The Flood Advisory is extended for the following rivers in Oklahoma... Cimarron River near Waynoka affecting Woods, Major and Woodward Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Cimarron River near Waynoka. * WHEN...Until early Tuesday morning. * IMPACTS...At 8.0 feet, Bankfull conditions exist along the river... and some overflows may occur over some low-lying areas near the river. The river reach affected extends from near Freedom upstream... to the U.S. Highway 281 crossing south of Little Sahara State Park near Waynoka... to near Orienta in Major County. * ADDITIONAL DETAILS... - At 7:30 PM CDT Saturday the stage was 7.5 feet. - Bankfull stage is 8.0 feet. - Forecast...The Cimarron River is expected to rise to a crest of 7.8 feet on Sunday evening. - Action stage is 7.5 feet. - Flood stage is 8.0 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 Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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