Weather Alert in Ohio
Flood Warning issued March 6 at 6:02PM EST until March 7 at 7:02AM EST by NWS Wilmington OH
AREAS AFFECTED: Greene, OH; Warren, OH
DESCRIPTION: ...The Flood Warning continues for the following rivers... Little Miami River at Spring Valley. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Little Miami River at Spring Valley. * WHEN...Until Saturday morning. * IMPACTS...At 12.0 feet, Water covers low-lying areas close to the river near Spring Valley, Roxanna and east of Waynesville. Water continues to flood Corwin Road, as well as Waynesville and Middletown Roads, along with Bellbrook golf driving range and portions of Washington Mill Park. * ADDITIONAL DETAILS... - At 5:00 PM EST Friday the stage was 12.0 feet. - Forecast...The river is not expected to drop below flood stage of 11 ft until after midnight. - Flood stage is 11.0 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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