Weather Alert in Oklahoma
Flood Warning issued May 27 at 9:03AM CDT until May 28 at 5:17AM CDT by NWS Tulsa OK
AREAS AFFECTED: Ottawa, OK
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Oklahoma... Deep Fork River near Beggs affecting Okmulgee County. Neosho River near Commerce affecting Ottawa County. Illinois River near Tahlequah affecting Cherokee County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Neosho River near Commerce. * WHEN...Until late tonight. * IMPACTS...At 15.0 feet, minor lowland flooding occurs. Low lying areas in Riverview Park experience minor flooding. * ADDITIONAL DETAILS... - At 8:30 AM CDT Tuesday the stage was 15.1 feet. - Forecast...The river is expected to rise to a crest of 15.5 feet this evening. It will then fall below flood stage late this evening. - Flood stage is 15.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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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