Weather Alert in Texas

Current Alerts for Dallas/Fort Worth International Airport, TX: Flood Watch

Flood Warning issued May 4 at 8:17PM CDT by NWS Shreveport LA

AREAS AFFECTED: Angelina, TX; Houston, TX; Polk, TX; Trinity, TX; Tyler, TX

DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Neches River Near Diboll affecting Houston, Trinity, Polk, Tyler and Angelina Counties. For the Neches River...including Lake Palestine, Neches, Alto, Diboll, Rockland...Minor flooding is forecast. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Neches River near Diboll. * WHEN...Until further notice. * IMPACTS...At 14.0 feet, Minor lowland flooding of boat ramps, paths, and trails. Move livestock and equipment to higher ground. * ADDITIONAL DETAILS... - At 7:15 PM CDT Sunday the stage was 14.6 feet. - Bankfull stage is 12.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:15 PM CDT Sunday was 14.7 feet. - Forecast...The Neches River southwest of Diboll is expected to continue a slow fall through midweek. However, additional rises are possible as heavy rainfall is expected over the Neches River basin Tuesday and Tuesday night. - Flood stage is 12.0 feet. - Flood History...This crest compares to a previous crest of 14.6 feet on 12/12/1998. - http://www.weather.gov/safety/flood

INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. 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. 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 evening at 900 PM CDT.

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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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