Weather Alert in Texas
Flood Warning issued April 23 at 9:08PM CDT by NWS Lake Charles LA
AREAS AFFECTED: Jasper, TX; Tyler, TX
DESCRIPTION: ...The National Weather Service in Lake Charles LA has issued a Flood Warning for the following rivers in Texas... Neches River Near Town Bluff For the Neches River...including Town Bluff, Evadale, Neches River Saltwater Barrier...Minor flooding is forecast. Additional information is available at www.weather.gov. The next statement will be issued Wednesday evening at 915 PM CDT. * WHAT...Minor flooding is forecast. * WHERE...Neches River near Town Bluff. * WHEN...From late Thursday night until further notice. * IMPACTS...At 70.0 feet, Flooding can be expected around Barlow Lake and Brushy Lake with some roads being cutoff and some of the lowest properties near the river begin to flood. * ADDITIONAL DETAILS... - At 8:00 PM CDT Tuesday the stage was 65.1 feet. - Forecast...The river is expected to rise to a crest of 69.7 feet early Saturday morning. - Flood stage is 68.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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
