Weather Alert in Oklahoma
Flood Warning issued June 17 at 3:13AM CDT until June 17 at 7:00PM CDT by NWS Norman OK
AREAS AFFECTED: Payne, OK
DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Cimarron River near Ripley affecting Payne County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Cimarron River near Ripley. * WHEN...Until this evening. * IMPACTS...At 17.0 feet, Places along the Cimarron River valley in Payne County are briefly flooded. Agricultural lands and oil wells located near the channel are isolated by water in cutoff channels along the river valley. * ADDITIONAL DETAILS... - At 3:00 AM CDT Tuesday the stage was 17.4 feet. - Bankfull stage is 17.0 feet. - Forecast...The Cimarron River is expected to fall below flood stage this afternoon and continue falling. - Flood stage is 17.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. 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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