Weather Alert in Mississippi
Flood Warning issued May 13 at 9:01AM CDT until May 15 at 7:00AM CDT by NWS Mobile AL
AREAS AFFECTED: George, MS; Greene, MS; Perry, MS
DESCRIPTION: ...The Flood Warning continues for the following rivers in Mississippi... Leaf Near McLain affecting George, Greene and Perry Counties. For the Leaf River...including McLain, New Augusta...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Leaf near McLain. * WHEN...Until Thursday morning. * IMPACTS...At 18.0 feet, Considerable flooding of agricultural and lowlands near the river. * ADDITIONAL DETAILS... - At 8:15 AM CDT Tuesday the stage was 18.6 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:15 AM CDT Tuesday was 18.6 feet. - Forecast...The river is expected to rise to a crest of 18.7 feet this afternoon. It will then fall below flood stage early Thursday morning. - Flood stage is 18.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/mob. Click on the Rivers and Lakes menu for forecasts and observations. The next statement will be issued when updates occur.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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