Weather Alert in Texas
Flood Advisory issued July 9 at 3:58PM CDT until July 9 at 6:00PM CDT by NWS San Angelo TX
AREAS AFFECTED: Concho, TX; McCulloch, TX; Menard, TX; San Saba, TX
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of west central Texas, including the following counties, Concho, McCulloch, Menard and San Saba. * WHEN...Until 600 PM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 354 PM CDT, Doppler radar indicated a band of showers and thunderstorms with heavy rain, moving south across SanSaba and McCulloch Counties. Rainfall of 1 to 1.5 inches is expected to occur in a short period of time, and this will cause minor flooding especially in low-lying areas, city streets and poor drainage places. Street flooding is likely in Brady and and San Saba. - Some locations that will experience flooding include... Brady, San Saba, Richland Springs, Algerita, Melvin, Rochelle, Placid, Voca, Sloan, Brady Lake, Lohn, Pear Valley, Salt Gap, Chappel, Bend, Hall, Us-190 Near The Mcculloch-San Saba County Line, Harkeyville and The Intersection Of Us-190 And Ranch Road 1311. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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