Weather Alert in Nebraska
Flood Warning issued September 1 at 7:32PM CDT until September 2 at 9:20PM CDT by NWS Omaha/Valley NE
AREAS AFFECTED: Saline, NE
DESCRIPTION: ...The National Weather Service in Omaha/Valley NE has issued a Flood Warning for the following rivers in Nebraska... Big Blue River Near Crete affecting Saline County. * WHAT...Minor flooding is forecast. * WHERE...Big Blue River near Crete. * WHEN...From this evening to late tomorrow evening. * IMPACTS...At 16.0 feet, Some rural lowlands begin to flood. At 18.0 feet, Additional flooding of lowland agricultural fields continues. * ADDITIONAL DETAILS... - At 6:45 PM CDT Monday the stage was 20.5 feet...or 0.5 feet below flood stage. - Bankfull stage is 18.0 feet. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 21.7 feet just after midnight tonight. It will then fall below flood stage early Tuesday morning. - Flood stage is 21.0 feet.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at water.noaa.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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