Weather Alert in Indiana
Flood Warning issued April 1 at 5:38AM EDT by NWS Northern Indiana
AREAS AFFECTED: Allen, IN; De Kalb, IN; Defiance, OH
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Ohio... Indiana... Tiffin River at Stryker affecting Williams, Defiance and Fulton OH Counties. Spy Run Creek at Park Drive At Fort Wayne Children's Zoo affecting Allen IN County. ...The Flood Warning continues for the following rivers in Ohio... Indiana... Saint Joseph River Ohio near Newville affecting De Kalb, Allen IN and Defiance Counties. For the Saint Joseph River Ohio...including Newville...Minor flooding is forecast. For the Tiffin River...including Stryker...Minor flooding is forecast. For the Spy Run Creek...including Park Drive At Fort Wayne Children's Zoo...Moderate flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Saint Joseph River Ohio near Newville. * WHEN...From this evening until further notice. * IMPACTS...At 12.0 feet, DeKalb County Road 42 about 3 miles northeast of Newville floods. Agricultural and low lands flood along the St. Joseph River to the Cedarville Reservoir. * ADDITIONAL DETAILS... - At 5:00 AM EDT Wednesday the stage was 10.3 feet. - Forecast...The river is expected to rise above flood stage this evening and continue rising to a crest of 12.7 feet Friday evening. - Flood stage is 12.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Detailed river forecasts and additional information can be found at www.weather.gov/iwx under Rivers and Lakes. The next statement will be issued this afternoon at 400 PM EDT.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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