Weather Alert in Texas
Severe Thunderstorm Warning issued August 2 at 3:38PM CDT until August 2 at 4:45PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Bell, TX; Milam, TX
DESCRIPTION: SVRFWD The National Weather Service in Fort Worth has issued a * Severe Thunderstorm Warning for... Central Milam County in central Texas... Southeastern Bell County in central Texas... * Until 445 PM CDT. * At 337 PM CDT, severe thunderstorms were located along a line extending from near Buckholts to near Rockdale to near Tanglewood, moving east at 10 mph. A second thunderstorm capable of producing severe winds was located 1 mile east of Little River-Academy, moving southeast at 20 mph. HAZARD...60 mph wind gusts and nickel size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Severe thunderstorms will be near... Rockdale, Buckholts, and Alcoa Lake around 345 PM CDT. Other locations impacted by these severe thunderstorms include Minerva, Ben Arnold, Cyclone, Sharp, Hoyte, Yarrelton, Pettibone, Milano, Silver City, and Edgeworth.
INSTRUCTION: For your protection get inside a sturdy structure and stay away from windows.
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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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