Weather Alert in Indiana

Recent Locations: Coarsegold, CA   Wellington, KS   Gosport, IN  

Flood Warning issued April 1 at 2:31AM EDT by NWS Northern Indiana

AREAS AFFECTED: Allen, IN; De Kalb, IN; Defiance, OH

DESCRIPTION: ...The National Weather Service in Northern Indiana has issued a Flood Warning for the following rivers in Ohio...Indiana... Saint Joseph River Ohio near Newville affecting De Kalb, Defiance and Allen IN Counties. Tiffin River at Stryker affecting Fulton OH, Williams and Defiance Counties. .Heavy rain has caused area rivers to rise. For the Saint Joseph River Ohio...including Newville...Minor flooding is forecast. For the Tiffin River...including Stryker...Minor 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 2:00 AM EDT Wednesday the stage was 9.2 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 evening at 845 PM EDT.

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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