Weather Alert in Texas
Severe Thunderstorm Warning issued August 28 at 5:38PM CDT until August 28 at 6:30PM CDT by NWS Shreveport LA
AREAS AFFECTED: Camp, TX; Upshur, TX; Wood, TX
DESCRIPTION: SVRSHV The National Weather Service in Shreveport has issued a * Severe Thunderstorm Warning for... Eastern Wood County in northeastern Texas... Upshur County in northeastern Texas... Southwestern Camp County in northeastern Texas... * Until 630 PM CDT. * At 538 PM CDT, severe thunderstorms were located along a line extending from 8 miles north of Gilmer to 6 miles northeast of Hainesville, moving southeast at 15 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect damage to roofs, siding, and trees. * Locations impacted include... Gilmer, Pittsburg, Hawkins, Diana, Rosewood, Midway, Perryville, Bettie, Grice, and Pritchett.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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