Weather Alert in Ohio
Flood Warning issued May 11 at 11:27AM EDT until May 12 at 12:00PM EDT by NWS Northern Indiana
AREAS AFFECTED: Defiance, OH; Fulton, OH; Williams, OH
DESCRIPTION: ...The Flood Warning continues for the following rivers in Ohio... Tiffin River at Stryker affecting Defiance, Fulton OH and Williams Counties. For the Tiffin River...including Stryker...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Tiffin River at Stryker. * WHEN...Until early tomorrow afternoon. * IMPACTS...At 12.0 feet, Portions of State Route 66 flood north of Archbold. * ADDITIONAL DETAILS... - At 11:00 AM EDT Sunday the stage was 12.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 11:00 AM EDT Sunday was 12.8 feet. - Forecast...The river is expected to fall below flood stage early tomorrow afternoon and continue falling to 6.8 feet Friday morning. - Flood stage is 11.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Detailed river forecasts and additional information can be found at www.weather.gov/iwx under Rivers and Lakes. The next statement will be issued late tonight at 530 AM 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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