Weather Alert in Texas
Special Weather Statement issued June 30 at 4:55PM CDT by NWS Austin/San Antonio TX
AREAS AFFECTED: Val Verde; Edwards
DESCRIPTION: At 454 PM CDT, Doppler radar was tracking strong thunderstorms along a line extending from 15 miles east of Carta Valley to 6 miles northeast of Long Point to 10 miles west of Cienegas Terrace. Movement was northwest at 35 mph. HAZARD...Wind gusts up to 50 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Del Rio, Comstock, Loma Alta, Lake View, Amistad Acres, Shumla, Carta Valley, Cienegas Terrace, Amistad Village, Black Brush Point, Seminole Canyon State Park, Box Canyon, Diablo East, Governors Landing, Long Point, Pecos River Boat Ramp, 277 South Boat Ramp, 277 North Campground, Rough Canyon Recreation Area, and Spur 406 Campground.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. If on or near Lake Amistad, get out of the water and move indoors or inside a vehicle. Remember, lightning can strike out to 10 miles from the parent thunderstorm. If you can hear thunder, you are close enough to be struck by lightning. Move to safe shelter now! Do not be caught on the water in a thunderstorm.
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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
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