Weather Alert in Texas
Flood Warning issued April 24 at 8:48PM CDT until April 28 at 10:36AM CDT by NWS Fort Worth TX
AREAS AFFECTED: Jack, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... West Fork Trinity River Near Jacksboro affecting Jack County. ...The Flood Warning is extended for the following rivers in Texas... West Fork Trinity River Near Boyd affecting Wise County. Denton Creek Near Justin affecting Denton County. * WHAT...Minor flooding is occurring and moderate flooding is forecast. * WHERE...West Fork Trinity River near Jacksboro. * WHEN...Until late Monday morning. * IMPACTS...At 22.0 feet, Moderate flooding along the river reach is expected. * ADDITIONAL DETAILS... - At 8:00 PM CDT Thursday the stage was 20.4 feet. - Bankfull stage is 18.0 feet. - Flood stage is 20.0 feet. - Forecast...The river is expected to rise to a crest of 22.5 feet tomorrow evening. It will then fall below flood stage late Sunday evening.
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. Additional information is available at www.water.noaa.gov/wfo/FWD.
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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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