Weather Alert in Texas
Severe Thunderstorm Warning issued September 5 at 7:09PM CDT until September 5 at 7:45PM CDT by NWS Fort Worth TX
AREAS AFFECTED: Collin, TX; Denton, TX
DESCRIPTION: At 708 PM CDT, a severe thunderstorm was located near Prosper, or 8 miles northwest of Frisco, moving east at 40 mph. Quarter to half dollar sized hail was observed between Denton and Prosper. HAZARD...65 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. This severe storm will be near... McKinney, Frisco, Prosper, and Celina around 715 PM CDT. Melissa around 725 PM CDT. Other locations impacted by this severe thunderstorm include Oak Point, Lincoln Park, Weston, Lewisville Lake, Lakewood Village, and Providence Village.
INSTRUCTION: For your protection stay inside a sturdy structure and keep away from windows. Continuous cloud to ground lightning is occurring with this storm. Move indoors immediately.
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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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