Weather Alert in Alabama

Recent Locations: Dallas, NC   Dripping Springs, TX   Cordova, AL  

Flood Watch issued August 2 at 11:47PM CDT until August 4 at 12:00AM CDT by NWS Birmingham AL

AREAS AFFECTED: Lowndes; Montgomery; Macon; Bullock; Lee; Russell; Pike; Barbour

DESCRIPTION: Periods of scattered to numerous showers and thunderstorms producing heavy rainfall are expected through Sunday. Due to the combination of slow movement and high rainfall rates, this activity will pose a threat of flash flooding. Additional rounds of showers and thunderstorms are likely on Monday. Depending on the forecast evolution of this activity, the Flood Watch may need to be extended into Monday for some counties in east Alabama. * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...A portion of central Alabama, including the following counties, Barbour, Bullock, Lee, Lowndes, Macon, Montgomery, Pike and Russell. * WHEN...Through Sunday evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Creeks and streams may rise out of their banks. * ADDITIONAL DETAILS... - 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 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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