Weather Alert in Texas
Flood Advisory issued June 10 at 5:06AM CDT until June 10 at 8:15AM CDT by NWS San Angelo TX
AREAS AFFECTED: Crockett, TX; Irion, TX; Schleicher, TX; Tom Green, TX
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of west central Texas, including the following counties, Crockett, Irion, Schleicher and Tom Green. * WHEN...Until 815 AM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 505 AM CDT, Doppler radar indicated heavy rain due to thunderstorms. Minor flooding is ongoing or expected to begin shortly in the advisory area. Between 0.75 and 1.25 inches of rain have fallen. - Additional rainfall amounts of 0.5 to 0.75 inches are expected over the area. This additional rain will result in minor flooding. - Some locations that will experience flooding include... Mertzon, Sherwood, Barnhart, Arden, Us-190 Near The Crockett- Sutton County Line and Us-67 Near The Irion-Tom Green County Line. - This includes the following Low Water Crossings... RM 853 crossing Dry Draw, Ranch Road 853 crossing east Rocky Creek, Ranch Road 859 crossing west Rocky Creek, Ranch Road 853 crossing Middle Concho River, County Road 113 crossing Dove Creek, crossings along County Road 411, crossings along County Road 302, County Road 202 crossing Lopez Creek, Sherwood Cemetery crossing and County Road 202 crossing Spring Creek. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding. Be aware of your surroundings and do not drive on flooded roads.
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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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