Weather Alert in Ohio
Flood Warning issued May 5 at 5:30AM EDT until May 7 at 8:00AM EDT by NWS Cleveland OH
AREAS AFFECTED: Holmes, OH; Wayne, OH
DESCRIPTION: ...The Flood Warning continues for the following rivers in Ohio... Killbuck Creek Near Killbuck affecting Wayne and Holmes Counties. For the Killbuck Creek...including Killbuck...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Killbuck Creek near Killbuck. * WHEN...Until Wednesday morning. * IMPACTS...At 16.0 feet, Flooded roads in and near Killbuck include Water Street, County Road 621, State Route 60 south, State Route 520, as well as local low lying roads. * ADDITIONAL DETAILS... - At 5:00 AM EDT Monday the stage was 15.9 feet. - Forecast...The river is expected to fall below flood stage early Wednesday morning and continue falling to 12.6 feet early Friday afternoon. - Flood stage is 15.0 feet. - Please visit www.weather.gov/safety/flood for flood safety and preparedness information.
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov/cle. The next statement will be issued this afternoon at 330 PM EDT.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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