Weather Alert in Texas
Flood Advisory issued July 9 at 4:16PM CDT until July 9 at 5:15PM CDT by NWS San Angelo TX
AREAS AFFECTED: Tom Green, TX
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of west central Texas, including the following county, Tom Green. * WHEN...Until 515 PM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 414 PM CDT, Doppler radar indicated a thunderstorm with very heavy rain due over the San Angelo Airport and the far southern part of San Angelo. The storm was moving slowly northeast at 10 mph. Rainfall up to one inch in a short period of time will cause street flooding, and minor flooding of low-lying and poor drainage areas. Minor flooding is ongoing or expected to begin shortly in the advisory area. - Some locations that will experience flooding include... San Angelo, Lake Nasworthy and Twin Buttes Reservoir. - 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 Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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