Weather Alert in Texas
Flood Warning issued June 13 at 9:25AM CDT until June 15 at 5:00AM CDT by NWS Houston/Galveston TX
AREAS AFFECTED: Brazoria, TX; Fort Bend, TX; Wharton, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... San Bernard River near Boling affecting Brazoria, Wharton and Fort Bend Counties. For the San Bernard River...including Sweeny, East Bernard, Boling... Moderate flooding is forecast. * WHAT...Moderate flooding is occurring and moderate flooding is forecast. * WHERE...San Bernard River near Boling. * WHEN...Until early Sunday morning. * IMPACTS...At 25.0 feet, Moderate lowland flooding continues with significant backwater flooding up Peach Creek and minor backwater flooding up West Bernard Creek in Wharton County. Backwater flooding up Snake Creek threatens low-lying areas in the Tierra Grande subdivision. * ADDITIONAL DETAILS... - At 8:15 AM CDT Friday the stage was 23.8 feet. - Bankfull stage is 14.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:15 AM CDT Friday was 23.9 feet. - Forecast...The river is expected to fall below flood stage tomorrow afternoon and continue falling to 4.7 feet Wednesday morning. - Flood stage is 18.0 feet. - Flood History...This crest compares to a previous crest of 23.8 feet on 06/03/1992. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/hgx. The next statement will be issued late tonight at 330 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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