Weather Alert in Alabama
Flood Watch issued August 13 at 8:17AM CDT until August 13 at 7:00PM CDT by NWS Huntsville AL
AREAS AFFECTED: Lauderdale; Limestone; Madison; Marshall; Jackson; DeKalb; Moore; Lincoln; Franklin
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Portions of Alabama, including the following areas, DeKalb, Jackson, Lauderdale, Limestone, Madison and Marshall and southern middle Tennessee, including the following areas, Franklin TN, Lincoln and Moore. * WHEN...Until 7 PM CDT this evening. * IMPACTS...Creeks and streams may rise out of their banks. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - Several rounds of rain and thunderstorms are expected to impact the Flood Watch area today. With soils becoming increasingly saturated, additional rainfall will quickly be converted to runoff, increasing the risk for flooding. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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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