Weather Alert in Texas
Flood Warning issued July 5 at 8:12AM CDT until July 7 at 3:06PM CDT by NWS Midland/Odessa TX
AREAS AFFECTED: Brewster, TX
DESCRIPTION: ...The Flood Warning continues for the following rivers in Texas... Rio Grande at Rio Grande at Presidio Vehicle Bridge affecting Presidio County. Rio Grande below Rio Grande below Rio Conchos near Presidio, Texas affecting Presidio County. Rio Grande at Rio Grande near Castolon, Texas affecting Brewster County. Rio Grande at Rio Grande at Rio Grande Village, BBNP, Texas affecting Brewster County. Rio Grande at Rio Grande at Johnson Ranch near Castolon, Texas affecting Brewster County. For the Rio Grande...including Rio Grande at Presidio Vehicle Bridge, Rio Grande below Rio Conchos near Presidio, Texas, Rio Grande near Castolon, Texas, Rio Grande at Johnson Ranch near Castolon, Texas, Rio Grande at Rio Grande Village, BBNP, Texas... Moderate flooding is forecast. * WHAT...Moderate flooding is occurring and moderate flooding is forecast. * WHERE...Rio Grande at Rio Grande at Rio Grande Village, BBNP, Texas. * WHEN...Until Monday afternoon. * IMPACTS...At 12.0 feet (3.7 meters), the river reaches bankfull, and no damage is expected. Preparations may be necessary to remove water pumps. The park should be notified at this time if additional rises are expected so they will have time to remove the pumps. At 13.0 feet (4.0 meters), the river reaches minor flood stage. Water reaches the water pumps maintained by the park service that are used to water the campgrounds and to provide water to the employee living quarters. It may be necessary for park personnel to remove the pumps. At 15.0 feet (4.6 meters), the river reaches moderate flood stage. Water pumps submerge. * ADDITIONAL DETAILS... - At 7:00 AM CDT Saturday the stage was 15.7 feet (4.8 meters). - Bankfull stage is 12.0 feet (3.7 meters). - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 AM CDT Saturday was 15.8 feet (4.8 meters). - Forecast...The river will rise to 16.4 feet (5.0 meters) late this afternoon. It will then fall below flood stage late tonight to 12.1 feet (3.7 meters) early tomorrow afternoon. It will rise to 12.3 feet (3.7 meters) tomorrow evening. It will then fall again and remain below flood stage. - Flood stage is 13.0 feet (4.0 meters). - Flood History...This crest compares to a previous crest of 16.5 feet (5.0 meters) on 05/28/2023. - http://www.weather.gov/safety/flood
INSTRUCTION: Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely. Caution is urged when walking near riverbanks. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued this evening at 815 PM CDT.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
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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.
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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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