Weather Alert in Texas
Flash Flood Warning issued August 30 at 3:22PM CDT until August 30 at 6:30PM CDT by NWS Midland/Odessa TX
AREAS AFFECTED: Jeff Davis, TX
DESCRIPTION: FFWMAF The National Weather Service in Midland/Odessa has issued a * Flash Flood Warning for... Central Jeff Davis County in southwestern Texas... * Until 630 PM CDT. * At 322 PM CDT, Doppler radar and automated rain gauges indicated thunderstorms producing heavy rain across the warned area. Between 1 to 2 inches of rain have fallen near McDonald Observatory. The expected rainfall rate is 1 to 3 inches in 1 hour. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar and automated gauges. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. * Some locations that will experience flash flooding include... Fort Davis, McDonald Observatory, Davis Mountains State Park, Bloys Camp, Black Mountain, Buffalo Trail Scout Camp, Indian Lodge, Fort Davis National Historical Site and Star Mountain. This includes the following streams and drainages... Big Aguja Canyon, South Fork Alamito Creek, Barrilla Draw, Alamito Creek, Madera Canyon, Cienega Creek, Cherry Creek, North Fork Cienega Creek, Cook Creek and Limpia Creek.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads. In hilly terrain there are hundreds of low water crossings which are potentially dangerous in heavy rain. Do not attempt to cross flooded roads. Find an alternate route.
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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
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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