Weather Alert in Texas
Flood Warning issued July 2 at 8:00PM CDT until July 3 at 7:00AM CDT by NWS Midland/Odessa TX
AREAS AFFECTED: Culberson, TX; Jeff Davis, TX
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is expected. * WHERE...A portion of southwest Texas, including the following counties, Culberson and Jeff Davis. * WHEN...Until 700 AM CDT /600 AM MDT/ Thursday. * IMPACTS...Several roads remain closed due to flooding. Low-water crossings are inundated with water and may not be passable. Additional heavy rainfall may lead to flash flooding. * ADDITIONAL DETAILS... - At 754 PM CDT /654 PM MDT/, Doppler radar indicated lingering showers over the warned area, but the overall intensity and coverage of rain has been decreasing since 7 PM CDT / 6 PM MDT. Several inches of rain has fallen over much of Jeff Davis and southeastern Culberson county the past couple of days. Some roads remain closed and low water crossings will remain inundated from the heavy rains through the overnight hours. - Some locations that will experience flooding include... Kent, Fort Davis, McDonald Observatory, Bloys Camp, Davis Mountains State Park, Black Mountain, Buffalo Trail Scout Camp, Indian Lodge, Fort Davis National Historical Site and Star Mountain. - http://www.weather.gov/safety/flood
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. In hilly terrain there are hundreds of low water crossings which are potentially dangerous in heavy rain. Do not attempt to cross flooded roads or barricades. Find an alternate route. Flooding is occurring or is imminent. It is important to know where you are relative to streams, rivers, or creeks which can become killers in heavy rains. Campers and hikers should avoid streams or creeks.
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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.
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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