Weather Alert in Ohio
Flood Warning issued March 3 at 10:28PM EST until March 5 at 10:00PM EST by NWS Wilmington OH
AREAS AFFECTED: Warren, OH
DESCRIPTION: ...The National Weather Service in Wilmington has issued a Flood Warning for the following rivers... Little Miami River near South Lebanon. * WHAT...Minor flooding is forecast. * WHERE...Little Miami River near South Lebanon. * WHEN...From Wednesday morning to late Thursday evening. * IMPACTS...At 21.0 feet, Flooding can be expected near Turtle Creek in South Lebanon. Roads affected by the flooding include Broadway, McKinley and Pike Streets, with expanded flooding along Mason-Morrow-Millgrove Road and in areas of Morrow. * ADDITIONAL DETAILS... - At 10:00 PM EST Tuesday the stage was 9.0 feet. - Forecast...The river will rise above flood stage late Wednesday morning to 20.7 feet early Wednesday afternoon. It will then fall below flood stage late Wednesday evening to 17.1 feet Thursday morning. It will rise above flood stage again to 19.1 feet early Thursday afternoon. It will then fall below flood stage again Thursday afternoon. - Flood stage is 19.0 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/iln.
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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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