Weather Alert in Texas
Wind Advisory issued March 14 at 1:32AM MDT until March 14 at 6:00PM MDT by NWS Midland/Odessa TX
AREAS AFFECTED: Pecos; Terrell; Chinati Mountains; Marfa Plateau; Central Brewster County; Chisos Basin; Presidio Valley; Lower Brewster County
DESCRIPTION: * WHAT...For the Blowing Dust Advisory, visibility between one-quarter and one mile in blowing dust expected. For the Wind Advisory, west winds 25 to 35 mph with gusts up to 55 mph expected. * WHERE...Central Brewster, Lower Brewster County, Pecos, and Terrell Counties, and Chinati Mountains, Chisos Basin, Marfa Plateau, and Presidio Valley. * WHEN...For the Blowing Dust Advisory, from 7 AM this morning to 9 PM CDT this evening. For the Wind Advisory, from 7 AM this morning to 7 PM CDT this evening. * IMPACTS...Hazardous driving conditions due to reduced visibility. In addition to reduced visibility, strong winds will be hazardous to trailers and other high-profile vehicles. Gusty winds may blow around unsecured objects.
INSTRUCTION: Persons with respiratory problems should make preparations to stay indoors until the storm passes. Be ready for a sudden drop in visibility to near zero. If you encounter blowing dust or blowing sand on the roadway or see it approaching, pull off the road as far as possible and put your vehicle in park. Turn the lights all the way off and keep foot off the brake pedal. Remember, 'Pull Aside, Stay Alive'. Slow down, use low-beam headlights, and leave plenty of distance between you and other vehicles. Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution and keep both hands on the steering wheel. Use caution when driving as blowing dust may reduce visibility.
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Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
