Weather Alert in Oklahoma
Flood Advisory issued August 28 at 2:28AM CDT until August 30 at 7:00AM CDT by NWS Norman OK
AREAS AFFECTED: Grant, OK; Kay, OK
DESCRIPTION: ...The National Weather Service in Norman has issued a Flood Advisory for the following rivers in Oklahoma... Salt Fork Arkansas River near Alva affecting Woods and Alfalfa Counties. Chikaskia River near Blackwell affecting Kay and Grant Counties. Cimarron River near Dover affecting Kingfisher and Logan Counties. * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...Chikaskia River near Blackwell. * WHEN...From early this morning to Saturday morning. * IMPACTS...At 28.0 feet, Low-lying streets may experience nuisance flooding in the northeastern portions of Blackwell. Farmlands and local roads in extreme northeastern Grant and Kay counties may be under shallow water depths for a few hours. Southeast of blackwell... Hubbard Road may be briefly covered by shallow depths of water near the river. * ADDITIONAL DETAILS... - At 1:30 AM CDT Thursday the stage was 2.7 feet. - Bankfull stage is 28.0 feet. - Forecast...The Chikaskia River is expected to rise to a crest of 27.9 feet early tomorrow afternoon. - Action stage is 26.0 feet. - Flood stage is 29.0 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
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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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