Weather Alert in Oklahoma
Flood Advisory issued June 7 at 8:41PM CDT until June 9 at 1:00AM CDT by NWS Norman OK
AREAS AFFECTED: Lincoln, OK; Oklahoma, OK; Pottawatomie, OK
DESCRIPTION: ...The National Weather Service in Norman has issued a Flood Advisory for the following rivers in Oklahoma... North Canadian River near Harrah affecting Oklahoma, Pottawatomie and Lincoln Counties. * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...North Canadian River near Harrah. * WHEN...From this evening to early Monday morning. * IMPACTS...At 11.0 feet, Shallow flooding of low-lying areas along the river may occur in eastern Oklahoma County... the southwest corner of Lincoln County... and northwestern Pottawatomie County. * ADDITIONAL DETAILS... - At 8:00 PM CDT Saturday the stage was 10.1 feet. - Bankfull stage is 14.0 feet. - Forecast...The North Canadian River is expected to rise to a crest of 11.3 feet tomorrow morning. - Action stage is 11.0 feet. - Flood stage is 14.0 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 Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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