Weather Alert in Texas
Flood Warning issued August 30 at 2:11AM CDT until August 30 at 6:00PM CDT by NWS Lubbock TX
AREAS AFFECTED: Lubbock, TX
DESCRIPTION: ...The National Weather Service in Lubbock TX has issued a Flood Warning for the following rivers in Texas... Double Mountain Fork Brazos near Lubbock 4ESE affecting Lubbock County. * WHAT...Minor flooding is occurring. * WHERE...Double Mountain Fork Brazos near Lubbock 4ESE. * WHEN...From early this morning to this evening. * IMPACTS...At 11.0 feet, Flooding over FM-835 just west of Buffalo Springs will likely require closure of the highway. Flooding of loop road around west end of Buffalo Springs Lake also likely. The onset of flooding at FM-835 may be delayed by 4 to 6 hours after the river gauge at Southeast Loop 289 exceeds 11 feet or about 1000 CFS. * ADDITIONAL DETAILS... - At 1:45 AM CDT Saturday the stage was 12.6 feet. - Bankfull stage is 10.0 feet. - Forecast...No forecast is available for this location. - Flood stage is 11.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Be especially cautious at night when it is harder to recognize the dangers of flooding. Additional information is available at www.weather.gov. The next statement will be issued this afternoon at 215 PM CDT.
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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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