Weather Alert in Texas
Flood Warning issued April 27 at 2:11PM CDT until April 28 at 10:45AM CDT by NWS Norman OK
AREAS AFFECTED: Wilbarger, TX
DESCRIPTION: ...The National Weather Service in Norman OK has issued a Flood Warning for the following rivers in Texas... Pease River near Vernon affecting Wilbarger County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Pease River near Vernon. * WHEN...From this afternoon to late tomorrow morning. * IMPACTS...At 15.0 feet, Brief... shallow flooding affects agricultural lands and low-lying roads along the Pease River in north Wilbarger County. * ADDITIONAL DETAILS... - At 1:00 PM CDT Sunday the stage was 15.0 feet. - Bankfull stage is 15.0 feet. - Forecast...The Pease River is expected to rise to a crest of 15.5 feet just after midnight tonight. It will then fall below flood stage late tonight. - Flood stage is 15.0 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 are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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