Weather Alert in Texas
Flood Warning issued August 30 at 4:49PM CDT until August 31 at 12:00PM CDT by NWS Lubbock TX
AREAS AFFECTED: Lubbock, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Double Mountain Fork Brazos near Lubbock 4ESE affecting Lubbock County. .High water is still present along the Double Mountain Fork Brazos River in southeastern Lubbock County from earlier heavy rainfall that fell Friday night through Saturday morning. Local officials reported up to two feet of water still over roadways near Buffalo Springs Lake. Additional heavy rainfall is possible through early Sunday morning which may prolong flooding impacts. * WHAT...Although the river has fallen below flood stage as of late Saturday afternoon, flooding impacts continue upstream of Buffalo Springs Lake. Local officials reported up to two feet of water over FM-835 just west of Buffalo Springs on Saturday afternoon, and impacts to roadways and low lying areas are expected to persist through early Sunday. * WHERE...Double Mountain Fork Brazos near Lubbock 4ESE. * WHEN...Until noon on Sunday. * ADDITIONAL DETAILS... - At 4:15 PM CDT Saturday the stage was 7.9 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. Flooding is already occurring. Most flood related deaths occur in automobiles. Do not attempt to cross water covered bridges, dips, or low water crossings. Never try to cross a flowing stream, even a small one, on foot. To escape rising water find another route over higher ground. Additional information is available at www.weather.gov/lub. The next statement will be issued by Sunday afternoon at noon CDT.
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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