Weather Alert in Texas
Flood Warning issued May 10 at 8:41PM CDT until May 15 at 8:00PM CDT by NWS Shreveport LA
AREAS AFFECTED: Smith, TX; Upshur, TX; Wood, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Sabine River Near Hawkins affecting Wood, Smith and Upshur Counties. For the Sabine River...including Mineola, Hawkins, Gladewater, Longview, Beckville, Logansport...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Sabine River near Hawkins. * WHEN...From late tonight to Thursday evening. * IMPACTS...At 25.0 feet, Minor lowland flooding of pastures and boatramps. Move livestock and equipment to higher ground. * ADDITIONAL DETAILS... - At 7:45 PM CDT Saturday the stage was 22.2 feet. - Bankfull stage is 22.0 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 26.4 feet Tuesday morning. It will then fall below flood stage early Thursday afternoon. - Flood stage is 23.0 feet.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. The next statement will be issued Sunday evening at 845 PM CDT.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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