Weather Alert in Texas
Severe Thunderstorm Warning issued March 5 at 6:41PM CST until March 5 at 7:30PM CST by NWS Lubbock TX
AREAS AFFECTED: Briscoe, TX; Hall, TX
DESCRIPTION: SVRLUB The National Weather Service in Lubbock Texas has issued a * Severe Thunderstorm Warning for... Northwestern Hall County in the Panhandle of Texas... Northeastern Briscoe County in the Panhandle of Texas... * Until 730 PM CST. * At 640 PM CST, a severe thunderstorm was located 7 miles northeast of Caprock Canyon State Park, moving northeast at 45 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Memphis, Caprock Canyon State Park, Brice, Lakeview, and Plaska Community.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until midnight CST for the Panhandle of Texas.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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