Weather Alert in Nebraska
Flood Warning issued September 1 at 7:37PM CDT until September 3 at 2:00AM CDT by NWS Omaha/Valley NE
AREAS AFFECTED: Saunders, NE
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Nebraska... Wahoo Creek At Ithaca affecting Saunders County. * WHAT...Moderate flooding is forecast. * WHERE...Wahoo Creek at Ithaca. * WHEN...Until early Wednesday morning. * IMPACTS...At 21.0 feet, Homes near the gage site may be threatened with the flood waters. At 22.0 feet, The access road south of town is likely to flood. In addition, a low spot along Highway 66 just east of the gage site will flood. * ADDITIONAL DETAILS... - At 7:15 PM CDT Monday the stage was 18.1 feet...or 0.9 feet below flood stage. - Bankfull stage is 19.0 feet. - Forecast...The river is expected to rise above flood stage this evening to a crest of 21.8 feet just after midnight tonight. It will then fall below flood stage tomorrow morning. - Flood stage is 19.0 feet.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Motorists should not attempt to drive around barricades or drive cars through flooded areas. 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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