Weather Alert in Texas
Severe Thunderstorm Warning issued April 1 at 10:10PM CDT until April 1 at 11:15PM CDT by NWS San Angelo TX
AREAS AFFECTED: Coke, TX; Runnels, TX; Tom Green, TX
DESCRIPTION: SVRSJT The National Weather Service in San Angelo has issued a * Severe Thunderstorm Warning for... Southeastern Coke County in west central Texas... North central Tom Green County in west central Texas... Northwestern Runnels County in west central Texas... * Until 1115 PM CDT. * At 1009 PM CDT, a severe thunderstorm was located near The Intersection Of Highway 208 And Ranch Road 2662, or 11 miles north of Grape Creek, moving east at 40 mph. HAZARD...70 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * This severe thunderstorm will be near... Tennyson around 1020 PM CDT. Bronte around 1025 PM CDT. Maverick around 1030 PM CDT. Norton around 1035 PM CDT. Other locations impacted by this severe thunderstorm include The Intersection Of Highway 208 And Ranch Road 2662 and Ballinger Lake.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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