Weather Alert in Ohio

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Current Alerts for Cleveland, OH: Wind Advisory

Flood Warning issued March 14 at 12:36PM EDT until March 16 at 8:00AM EDT by NWS Northern Indiana

AREAS AFFECTED: Williams, OH

DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana...Ohio... Saint Joseph River Ohio near Newville affecting De Kalb, Defiance and Allen IN Counties. Saint Joseph River Ohio below Montpelier affecting Williams County. ...The Flood Warning continues for the following rivers in Ohio... Tiffin River at Stryker affecting Williams, Defiance and Fulton OH Counties. For the Saint Joseph River Ohio...including Montpelier, Newville... Moderate flooding is forecast. For the Tiffin River...including Stryker...Minor flooding is forecast. * WHAT...Moderate flooding is occurring and minor flooding is forecast. * WHERE...Saint Joseph River Ohio below Montpelier. * WHEN...Until Monday morning. * IMPACTS...At 13.0 feet, County Road K, one mile southwest of Montpelier begins to flood. Some flooding begins to affect the village of Pioneer. Significant low land and agricultural flooding occurs near the river. * ADDITIONAL DETAILS... - At 9:00 AM EDT Friday, March 13 the stage was 13.2 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 9:00 AM EDT Friday was -9999.0 feet. - Forecast...The river is expected to fall below flood stage tomorrow morning and continue falling to 10.5 feet Thursday morning. - 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 Sunday morning at 645 AM EDT.

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

Stratocumulus Clouds Next Topic: Stratus Clouds

Stratocumulus clouds are similar to altocumulus clouds in their fluffy appearance, but have a slightly darker shade due to their additional mass.

A good way to distinguish the two cloud types is to hold your hand out and measure the size of an individual cloud; if it is the size of your thumb it is generally an altocumulus cloud, if it is the size of your hand it is generally a stratocumulus cloud.

It is uncommon for stratocumulus clouds to produce precipitation, but if they do it is usually a light rain or snow.

Next Topic: Stratus Clouds

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

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