Weather Alert in Iowa
Flood Warning issued August 1 at 9:15PM CDT until August 3 at 6:00AM CDT by NWS Quad Cities IA IL
AREAS AFFECTED: Cedar, IA; Jones, IA; Linn, IA
DESCRIPTION: ...The National Weather Service in Quad Cities IA IL has issued a Flood Warning for the following rivers in Iowa... Wapsipinicon River near Anamosa Shaw Rd affecting Jones, Linn and Cedar Counties. * WHAT...Minor flooding is forecast. * WHERE...Wapsipinicon River near Anamosa Shaw Rd. * WHEN...From Saturday morning to Sunday morning. * IMPACTS...At 14.5 feet, Flood Stage. Lead Mine Road is completely covered. * ADDITIONAL DETAILS... - At 8:15 PM CDT Friday the stage was 13.7 feet. - Forecast...The river is expected to rise above flood stage late tomorrow morning to a crest of 14.6 feet early tomorrow afternoon. It will then fall below flood stage late tomorrow evening. - Flood stage is 14.5 feet.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/quadcities. The next statement will be issued by Saturday evening at 915 PM CDT.
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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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