Weather Alert in Texas
Flood Watch issued July 5 at 7:31PM CDT until July 6 at 7:00PM CDT by NWS San Angelo TX
AREAS AFFECTED: Coleman; Brown
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...A portion of west central Texas, including the following counties, Brown and Coleman. * WHEN...Through Sunday evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - Scattered showers and thunderstorms are expected to increase in coverage across Brown and Coleman Counties overnight. Pockets of heavy rainfall will be possible, with some locations seeing totals of 3 to 5 inches late tonight into Sunday. A few locations may see even heavier totals. Although Brown and Coleman did not see the heaviest rainfall over the last week, this much rain on soils that are already saturated will still lead to flash flooding.
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued. Flash flooding can be especially dangerous. Make sure you have a way of receiving warnings during the overnight hours.
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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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