Weather Alert in Mississippi

Recent Locations: Belen, MS   Corinth, MS  

Flood Warning issued May 9 at 10:00AM CDT until May 12 at 7:00PM CDT by NWS Jackson MS

AREAS AFFECTED: Madison, MS; Yazoo, MS

DESCRIPTION: ...The Flood Warning continues for the following rivers in Mississippi... Big Black River Near Bentonia affecting Yazoo and Madison Counties. Big Black River Near Bovina affecting Hinds and Warren Counties. Big Black River At West affecting Attala and Holmes Counties. * WHAT...Minor flooding is forecast. * WHERE...Big Black River near Bentonia. * WHEN...From late Sunday night to Monday evening. * IMPACTS...At 22.0 feet, Low lying woodland areas along the river begin to flood. * ADDITIONAL DETAILS... - At 9:00 AM CDT Friday the stage was 17.8 feet. - Forecast...The river is expected to rise to a crest of 22.0 feet early Monday morning. - Flood stage is 22.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.water.noaa.gov/wfo/jan The next statement will be issued this evening at 1000 PM CDT.

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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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