Weather Alert in Texas
Severe Thunderstorm Warning issued April 29 at 3:58PM CDT until April 29 at 5:00PM CDT by NWS Lubbock TX
AREAS AFFECTED: Crosby, TX; Dickens, TX; Garza, TX; Kent, TX; Lynn, TX
DESCRIPTION: SVRLUB The National Weather Service in Lubbock Texas has issued a * Severe Thunderstorm Warning for... Northwestern Kent County in northwestern Texas... Southern Dickens County in northwestern Texas... Southeastern Lynn County in northwestern Texas... Garza County in northwestern Texas... Southeastern Crosby County in northwestern Texas... * Until 500 PM CDT. * At 357 PM CDT, severe thunderstorms were located along a line extending from 4 miles east of Kalgary to 12 miles south of Grassland, moving east at 10 mph. HAZARD...Tennis ball size hail and 60 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Justiceburg, White River Lake, Lake Alan Henry, Kalgary, Spur, and Post.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Torrential rainfall is occurring with these storms, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.
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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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