Weather Alert in Ohio
Flood Warning issued May 8 at 7:45PM EDT until May 12 at 11:00PM 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 Fulton OH, Defiance 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 late Monday evening. * IMPACTS...At 13.0 feet, Flood waters begin to affect some farm buildings near Stryker and flood some secondary roads. * ADDITIONAL DETAILS... - At 7:00 PM EDT Thursday the stage was 13.4 feet. - Forecast...The river is expected to rise to a crest of 13.5 feet just after midnight tonight. It will then fall below flood stage late Sunday evening. - 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 Friday afternoon at 145 PM EDT.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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