Weather Alert in Oklahoma
Flood Warning issued June 10 at 2:05PM CDT until June 11 at 7:00AM CDT by NWS Norman OK
AREAS AFFECTED: Major, OK; Woods, OK; Woodward, OK
DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Cimarron River near Waynoka affecting Major, Woods and Woodward Counties. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Cimarron River near Waynoka. * WHEN...Until tomorrow morning. * IMPACTS...At 8.0 feet, Bankfull conditions exist along the river... and some overflows may occur over some low-lying areas near the river. The river reach affected extends from near Freedom upstream... to the U.S. Highway 281 crossing south of Little Sahara State Park near Waynoka... to near Orienta in Major County. * ADDITIONAL DETAILS... - At 1:30 PM CDT Tuesday the stage was 8.2 feet. - Bankfull stage is 8.0 feet. - Forecast...The Cimarron River is expected to fall below flood stage just after midnight tonight and continue falling. - Flood stage is 8.0 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 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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