Weather Alert in Oklahoma
Flood Advisory issued June 18 at 8:30PM CDT until June 20 at 1:00PM CDT by NWS Norman OK
AREAS AFFECTED: Kingfisher, OK; Logan, OK
DESCRIPTION: ...The Flood Advisory continues for the following rivers in Oklahoma... Cimarron River near Dover affecting Kingfisher and Logan Counties. * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Cimarron River near Dover. * WHEN...Until early Friday afternoon. * IMPACTS...At 17.0 feet, Rural lands and roads are covered by flood depths averaging almost a foot across Kingfisher County... and into western Logan County. Oil wells in lower places near the river channel are flooded or isolated. Livestock may become stranded by deeper flows in cutoff channels crossing the flood plain. Sandpit facilities near Dover could be flooded. * ADDITIONAL DETAILS... - At 7:30 PM CDT Wednesday the stage was 15.8 feet. - Bankfull stage is 17.0 feet. - Forecast...The Cimarron River is expected to rise to a crest of 16.8 feet tomorrow morning. - Action stage is 15.0 feet. - Flood stage is 17.0 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 is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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