Weather Alert in Oklahoma
Flood Watch issued April 29 at 8:50AM CDT until May 1 at 5:30PM CDT by NWS Norman OK
AREAS AFFECTED: Seminole; Hughes
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Watch for the following rivers in Oklahoma... Little River near Sasakwa affecting Seminole and Hughes Counties. * WHAT...Flooding is possible. * WHERE...Little River near Sasakwa. * WHEN...From Wednesday afternoon to Thursday afternoon. * IMPACTS...At 27.0 feet, Flood depths to about 1 foot of croplands and pastures along the Little River extending from near the State Highway 99 bridge to north of Sasakwa in Seminole County... to the confluence with the Canadian River in Hughes County. Floodwaters cover State Highway 99 near the river and south of Bowlegs. * ADDITIONAL DETAILS... - At 8:30 AM CDT Tuesday the stage was 8.3 feet. - Forecast...Flood stage may be reached early tomorrow afternoon. - Flood stage is 26.0 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 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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