Weather Alert in Ohio
Flood Warning issued May 10 at 10:43PM EDT until May 13 at 8:00AM EDT by NWS Northern Indiana
AREAS AFFECTED: Defiance, OH; Fulton, OH; Williams, OH
DESCRIPTION: ...The Flood Warning is extended 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 Tuesday morning. * IMPACTS...At 12.0 feet, Portions of State Route 66 flood north of Archbold. * ADDITIONAL DETAILS... - At 10:00 PM EDT Saturday the stage was 12.5 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 10:00 PM EDT Saturday was 13.1 feet. - Forecast...The river is expected to fall below flood stage late Monday morning and continue falling to 7.3 feet Thursday 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 Sunday afternoon at 445 PM EDT.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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