Weather Alert in Tennessee
Flood Warning issued June 16 at 9:29PM CDT until June 17 at 7:00PM CDT by NWS Memphis TN
AREAS AFFECTED: Crockett, TN; Dyer, TN; Lauderdale, TN
DESCRIPTION: ...The Flood Warning continues for the following rivers in Tennessee... South Fork of the Forked Deer near Halls For the South Fork Forked Deer River...including Jackson, Halls... Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...South Fork of the Forked Deer near Halls. * WHEN...Until tomorrow evening. * IMPACTS...At 9.0 feet, Farmland near the river is flooded. * ADDITIONAL DETAILS... - At 9:00 PM CDT Monday the stage was 9.6 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 9:00 PM CDT Monday was 9.7 feet. - Forecast...The river is expected to fall below flood stage early tomorrow afternoon and continue falling to 2.0 feet Saturday evening. - Flood stage is 9.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Caution is urged when walking near riverbanks. Additional information is available at weather.gov/memphis. The next statement will be issued as needed.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - 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
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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