Weather Alert in Texas
Flood Warning issued March 15 at 9:32AM CDT until March 21 at 10:00AM CDT by NWS Shreveport LA
AREAS AFFECTED: Angelina, TX; Nacogdoches, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Angelina River Near Angelina River at Hwy 59 near Lufkin affecting Nacogdoches and Angelina Counties. For the Angelina River...including Angelina River near Alto, Angelina River at Hwy 59 near Lufkin...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Angelina River near Angelina River at Hwy 59 near Lufkin. * WHEN...Until Saturday morning. * IMPACTS...At 161.0 feet, Expect minor flooding with the gravel parking lot flooded and water beginning to overflow the gravel road where it widens into the parking lot. Also expect about a foot of overflow across the left bank of the Angelina River looking downstream. * ADDITIONAL DETAILS... - At 8:45 AM CDT Sunday the stage was 161.2 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:45 AM CDT Sunday was 161.3 feet. - Forecast...The river is expected to rise to a crest of 161.8 feet Tuesday evening. It will then fall below flood stage late Thursday evening. - Flood stage is 161.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. Motorists should not attempt to drive around barricades or drive cars through flooded areas. Caution is urged when walking near riverbanks. For more hydrologic information, copy and paste the following website address into your favorite web browser URL bar: https://water.noaa.gov/wfo/SHV The next statement will be issued Monday morning at 945 AM CDT.
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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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